{"pageNumber":"231","pageRowStart":"5750","pageSize":"25","recordCount":11004,"records":[{"id":70238572,"text":"70238572 - 2005 - Coordinating NEHRP Post-Earthquake Investigations: Exercising the Plan","interactions":[],"lastModifiedDate":"2022-11-29T20:27:29.708001","indexId":"70238572","displayToPublicDate":"2005-11-01T14:23:36","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1436,"text":"Earthquake Spectra","active":true,"publicationSubtype":{"id":10}},"title":"Coordinating NEHRP Post-Earthquake Investigations: Exercising the Plan","docAbstract":"<p>Three exercises of The Plan to Coordinate NEHRP Post-Earthquake Investigations were developed and implemented in late 2003 and early 2004 in order to test the Plan itself via realistic scenarios, and for the NEHRP agencies to learn how to coordinate post-earthquake investigations. The exercises were selected to cover a range of seismic activity and consequences, and were based on scenario events: (1) a Hayward Fault Mw 7 event without foreshocks; (2) a New Madrid seismic zone Mw 7 event with foreshocks, and (3) a Puerto Rico Mw 8 subduction event on the Puerto Rican Trench accompanied by a tsunami affecting the eastern seaboard of the United States. Each exercise consisted of a four-hour telephone conference call with a Web-based electronic link and post-exercise evaluations fed back to participants. Evaluation of the exercises found the Plan to be adequate, with implementation of the Plan by the NEHRP agencies improving with each exercise. Based on the exercises, recommendations were provided that a Plan coordinator should be designated within USGS, an annual exercise of the Plan should be conducted in different regions of the United States, a permanent NEHRP electronic link should be created, and coordination of post-earthquake data collection, preservation, archiving, and dissemination should be greatly improved.</p>","language":"English","publisher":"SAGE Publishing","doi":"10.1193/1.2087707","usgsCitation":"Holzer, T.L., Scawthorn, C., and Rojahn, C., 2005, Coordinating NEHRP Post-Earthquake Investigations: Exercising the Plan: Earthquake Spectra, v. 21, no. 4, p. 1043-1062, https://doi.org/10.1193/1.2087707.","productDescription":"20 p.","startPage":"1043","endPage":"1062","costCenters":[],"links":[{"id":409815,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"4","noUsgsAuthors":false,"publicationDate":"2005-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Holzer, Thomas L. tholzer@usgs.gov","contributorId":2829,"corporation":false,"usgs":true,"family":"Holzer","given":"Thomas","email":"tholzer@usgs.gov","middleInitial":"L.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":857952,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scawthorn, Charles","contributorId":65755,"corporation":false,"usgs":true,"family":"Scawthorn","given":"Charles","affiliations":[],"preferred":false,"id":857953,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rojahn, Christopher","contributorId":41482,"corporation":false,"usgs":true,"family":"Rojahn","given":"Christopher","email":"","affiliations":[],"preferred":true,"id":857954,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70206128,"text":"70206128 - 2005 - Stratigraphy and structural history of the eastern edge of the Helena salient, Montana","interactions":[],"lastModifiedDate":"2019-10-24T06:36:48","indexId":"70206128","displayToPublicDate":"2005-10-23T14:39:47","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5878,"text":"The Journal of the Tobacco Root Geological Society","active":true,"publicationSubtype":{"id":10}},"title":"Stratigraphy and structural history of the eastern edge of the Helena salient, Montana","docAbstract":"<p>No abstract available.</p>","conferenceTitle":"TRGS 30th Annual Field Conference","conferenceLocation":"Sun River-Choteau, MT","language":"English","publisher":"Tobacco Root Geological Society Inc.","issn":"0096-7769","usgsCitation":"Reynolds, M.W., 2005, Stratigraphy and structural history of the eastern edge of the Helena salient, Montana: The Journal of the Tobacco Root Geological Society, v. 34, p. 109-118.","productDescription":"10 p.","startPage":"109","endPage":"118","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":368525,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Montana","city":"Helena","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.91748046874999,\n              46.13417004624326\n            ],\n            [\n              -111.3134765625,\n              46.13417004624326\n            ],\n            [\n              -111.3134765625,\n              46.912750956378915\n            ],\n            [\n              -112.91748046874999,\n              46.912750956378915\n            ],\n            [\n              -112.91748046874999,\n              46.13417004624326\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"34","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Reynolds, Mitchell W. 0000-0002-9966-3896 mwreynol@usgs.gov","orcid":"https://orcid.org/0000-0002-9966-3896","contributorId":4641,"corporation":false,"usgs":true,"family":"Reynolds","given":"Mitchell","email":"mwreynol@usgs.gov","middleInitial":"W.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":773677,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72478,"text":"ofr20051336 - 2005 - Known or suggested Quaternary tectonic faulting, central and eastern United States-new and updated assessments for 2005","interactions":[],"lastModifiedDate":"2012-02-02T00:13:57","indexId":"ofr20051336","displayToPublicDate":"2005-10-14T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1336","title":"Known or suggested Quaternary tectonic faulting, central and eastern United States-new and updated assessments for 2005","language":"ENGLISH","doi":"10.3133/ofr20051336","usgsCitation":"Wheeler, R.L., 2005, Known or suggested Quaternary tectonic faulting, central and eastern United States-new and updated assessments for 2005 (Online only, Version 1.0): U.S. Geological Survey Open-File Report 2005-1336, 40 p., https://doi.org/10.3133/ofr20051336.","productDescription":"40 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":191205,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7536,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1336/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only, Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4778","contributors":{"authors":[{"text":"Wheeler, Russell L. wheeler@usgs.gov","contributorId":858,"corporation":false,"usgs":true,"family":"Wheeler","given":"Russell","email":"wheeler@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":false,"id":285719,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72470,"text":"sim2841 - 2005 - Geologic map of the Stafford quadrangle, Stafford County, Virginia","interactions":[],"lastModifiedDate":"2022-04-14T18:57:29.415324","indexId":"sim2841","displayToPublicDate":"2005-10-13T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2841","title":"Geologic map of the Stafford quadrangle, Stafford County, Virginia","docAbstract":"Introduction\r\n\r\nThe Stafford 7.5-minute quadrangle, comprising approximately 55 square miles (142.5 square kilometers) of northeastern Virginia, is about 40 miles (mi) south of Washington, D.C. The region's main north-south transportation corridor, which connects Washington, D.C., and Richmond, Va., consists of Interstate 95, U.S. Highway 1, and the heavily used CSX and Amtrak railroads. Although the northern and eastern parts of the Stafford quadrangle have undergone extensive suburban development, the remainder of the area is still dominantly rural in character. The town of Stafford is the county seat.\r\n\r\nThe Stafford 7.5-minute quadrangle is located in the Fredericksburg 30'x60' quadrangle, where information on the regional stratigraphy and structure is available from Mixon and others' (2000) geologic map and multichapter explanatory text. In addition to straddling the 'Fall Zone' boundary between the Appalachian Piedmont and the Atlantic Coastal Plain provinces, this quadrangle contains the best preserved and best studied segment of the Stafford fault system, an important example of late Cenozoic faulting in eastern North America (Mixon and Newell, 1977). This 1:24,000-scale geologic map provides a detailed framework for interpreting and integrating topical studies of that fault system.\r\n\r\nOur geologic map integrates more than two decades of intermittent geologic mapping and related investigations by the authors in this part of the Virginia Coastal Plain. Earlier mapping in the Piedmont by Pavlides (1995) has been revised by additional detailed mapping in selected areas, particularly near Abel Lake and Smith Lake, and by field evaluation of selected contact relations.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sim2841","usgsCitation":"Mixon, R.B., Pavlides, L., Horton, J., Powars, D.S., and Schindler, J.S., 2005, Geologic map of the Stafford quadrangle, Stafford County, Virginia: U.S. Geological Survey Scientific Investigations Map 2841, 1 Plate: 57.00 x 34.00 inches, https://doi.org/10.3133/sim2841.","productDescription":"1 Plate: 57.00 x 34.00 inches","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":191017,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":110724,"rank":700,"type":{"id":7,"text":"Companion Files"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_81183.htm","linkFileType":{"id":5,"text":"html"},"description":"81183"},{"id":398745,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_81183.htm"},{"id":9491,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sim/2005/2841/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Virginia","county":"Stafford County","otherGeospatial":"Stafford quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.5,\n              38.375\n            ],\n            [\n              -77.375,\n              38.375\n            ],\n            [\n              -77.375,\n              38.5\n            ],\n            [\n              -77.5,\n              38.5\n            ],\n            [\n              -77.5,\n              38.375\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a841f","contributors":{"authors":[{"text":"Mixon, Robert B.","contributorId":50517,"corporation":false,"usgs":true,"family":"Mixon","given":"Robert","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":285708,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pavlides, Louis","contributorId":79444,"corporation":false,"usgs":true,"family":"Pavlides","given":"Louis","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":285709,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Horton, J. Wright Jr. 0000-0001-6756-6365 whorton@usgs.gov","orcid":"https://orcid.org/0000-0001-6756-6365","contributorId":423,"corporation":false,"usgs":true,"family":"Horton","given":"J. Wright","suffix":"Jr.","email":"whorton@usgs.gov","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":false,"id":285705,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Powars, David S. 0000-0002-6787-8964 dspowars@usgs.gov","orcid":"https://orcid.org/0000-0002-6787-8964","contributorId":1181,"corporation":false,"usgs":true,"family":"Powars","given":"David","email":"dspowars@usgs.gov","middleInitial":"S.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":285706,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schindler, J. Stephen 0000-0001-9550-5957 sschindl@usgs.gov","orcid":"https://orcid.org/0000-0001-9550-5957","contributorId":3270,"corporation":false,"usgs":true,"family":"Schindler","given":"J.","email":"sschindl@usgs.gov","middleInitial":"Stephen","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":285707,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70205865,"text":"70205865 - 2005 - National Acid Precipitation Assessment Program Report to Congress: An integrated assessment","interactions":[{"subject":{"id":70205862,"text":"70205862 - 2005 - Results of the acid rain program: Status and trends of emissions and environmental impacts (1990–2002)","indexId":"70205862","publicationYear":"2005","noYear":false,"chapter":"2","title":"Results of the acid rain program: Status and trends of emissions and environmental impacts (1990–2002)"},"predicate":"IS_PART_OF","object":{"id":70205865,"text":"70205865 - 2005 - National Acid Precipitation Assessment Program Report to Congress: An integrated assessment","indexId":"70205865","publicationYear":"2005","noYear":false,"title":"National Acid Precipitation Assessment Program Report to Congress: An integrated assessment"},"id":1},{"subject":{"id":70205863,"text":"70205863 - 2005 - Assessing acid deposition: Advances in the state of science","indexId":"70205863","publicationYear":"2005","noYear":false,"chapter":"3","title":"Assessing acid deposition: Advances in the state of science"},"predicate":"IS_PART_OF","object":{"id":70205865,"text":"70205865 - 2005 - National Acid Precipitation Assessment Program Report to Congress: An integrated assessment","indexId":"70205865","publicationYear":"2005","noYear":false,"title":"National Acid Precipitation Assessment Program Report to Congress: An integrated assessment"},"id":2}],"lastModifiedDate":"2019-10-09T07:15:17","indexId":"70205865","displayToPublicDate":"2005-10-08T16:27:32","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":5871,"text":"Report to Congress","active":true,"publicationSubtype":{"id":1}},"title":"National Acid Precipitation Assessment Program Report to Congress: An integrated assessment","docAbstract":"<p>Acid deposition, more commonly known as acid rain,&nbsp;occurs when emissions of sulfur dioxide (SO2) and nitrogen&nbsp;oxides (NOx) react in the atmosphere (with water, oxygen,&nbsp;and oxidants) to form various acidic compounds. These&nbsp;acidic compounds then fall to earth in either a wet form&nbsp;(rain, snow, and fog) or a dry form (gases, aerosols, and&nbsp;particles). Prevailing winds transport the acidic compounds&nbsp;hundreds of miles, often across state and national borders.&nbsp;At certain levels the acidic compounds, including small particles such as sulfates and nitrates can cause many negative&nbsp;human health and environmental effects. While ecosystems&nbsp;are subject to many stresses, including land-use changes,&nbsp;climate change, and variations in hydrologic and meteorologic cycles, the scientific literature has clearly demonstrated&nbsp;that these pollutants can:<br>• Degrade air quality,<br>• Impair visibility,<br>• Damage public health,<br>• Acidify lakes and streams,<br>• Harm sensitive forests,<br>• Harm sensitive coastal ecosystems, and<br>• Accelerate the decay of building materials, paints, and&nbsp;cultural artifacts such as buildings, statues, and&nbsp;sculptures.<br></p><p>Title IV was passed by Congress as part of the 1990 Clean&nbsp;Air Act Amendments to reduce emissions of SO<sub>2</sub> and NO<sub>x&nbsp;</sub>from fossil fuel-burning power plants in order to protect<br>ecosystems suffering damage from acid deposition and to&nbsp;improve air quality. At the same time, the National Acid&nbsp;Precipitation Assessment Program (NAPAP) was asked to&nbsp;periodically assess and report to Congress on the&nbsp;implementation of the Acid Rain Program, recent scientific&nbsp;knowledge surrounding acid deposition and its effects, and<br>the reduction in acid deposition necessary to prevent&nbsp;adverse ecological effects. This NAPAP Report focuses primarily on emission reductions from power plants, both in&nbsp;terms of assessing past reductions under the Acid Rain&nbsp;Program and in projecting the ecological effects of additional reductions of SO<sub>2</sub> and NO<sub>x</sub>. </p><p>It should be noted that power generation&nbsp;currently contributes approximately 69% of&nbsp;the SO<sub>2</sub> emissions and 22% of the NO<sub>x</sub> emissions nationwide. This contribution is&nbsp;decreasing as emissions from power generation continue to decrease, making the other&nbsp;sources of these pollutants more prominent.&nbsp;Modeling suggests that even if SO<sub>2</sub><br>emissions from power generation were&nbsp;reduced to zero, some lakes and streams&nbsp;would remain acidic due to acid deposition.&nbsp;However, there are several other regulations&nbsp;that reduce emissions of SO<sub>2</sub> and NO<sub>x</sub> from&nbsp;these non-power generation sources, such&nbsp;as the Tier II mobile source standards, the&nbsp;Heavy Duty Diesel standards, and the Clean&nbsp;Air Non-Road Diesel Rule, that have also&nbsp;been promulgated since 1990. These regulations, primarily designed to bring counties&nbsp;into attainment with fine particle and ozone&nbsp;air quality standards, also incidentally reduce&nbsp;emissions that contribute to acid deposition.</p><p>Implementation of Title IV has successfully&nbsp;and substantially reduced emissions of SO<sub>2&nbsp;</sub>and NO<sub>x</sub> from power generation at a significantly lower cost than expected:<br>• In 2002, SO<sub>2</sub> emissions were 10.2 million&nbsp;tons, 35% lower than 1990 emissions and&nbsp;40% lower than 1980 emissions.*<br>• In 2002, NO<sub>x</sub> emissions were 4.5 million&nbsp;tons, 33% lower than 1990 emissions.<br></p><p>In addition, SO<sub>2</sub> emissions from all sources&nbsp;have decreased by 32% since 1990 and&nbsp;emissions of NO<sub>x</sub> from all sources have&nbsp;decreased by 12% since 1990. Power generating sources continue to close in on the&nbsp;goal of reducing power plant SO<sub>2</sub> emissions&nbsp;from 1980 levels by 50% (to 8.95 million&nbsp;tons) as required by the 1990 Clean Air Act.&nbsp;Power generating sources have also exceed­ed the goal of a two million ton reduction in&nbsp;NO<sub>x</sub> emissions from projected 2000 levels&nbsp;as required by the 1990 Clean Air Act.<br></p><p>These emission reductions have contributed&nbsp;to measurable improvements in air quality,&nbsp;reductions in acid deposition, and the beginnings of recovery of acid-sensitive waters in&nbsp;some areas:<br>• SO2 concentrations in the atmosphere (a&nbsp;precursor to fine particles and acid deposition) have decreased since 1990. Average&nbsp;annual SO2 concentrations in the&nbsp;Northeast in 2000–2002 were 40% lower&nbsp;than they were in 1989–1991, concentrations in the mid-Atlantic were 30% lower,&nbsp;concentrations in the Southeast were 35%&nbsp;lower, and concentrations in the Midwest&nbsp;were 45% lower.<br>• Sulfate concentrations in the atmosphere (a major component of fine particles, especially in the East) have&nbsp;decreased since 1990 as well. Average&nbsp;annual sulfate concentrations in the&nbsp;Northeast and Midwest in 2000–2002&nbsp;were approximately 30% lower than they were in&nbsp;1989–1991, and concentrations in the mid-Atlantic and&nbsp;Southeast were 25% lower.<br>• Wet sulfate deposition, a major component of acid rain,&nbsp;has also decreased since 1990. Average annual sulfate&nbsp;deposition in the Northeast in 2000–2002 was 40% lower&nbsp;than it was in 1989–1991, deposition in the mid-Atlantic&nbsp;and Midwest was 35% lower, and deposition in the&nbsp;Southeast was 25% lower.<br>• Wet nitrate deposition has not decreased regionally from&nbsp;historical levels because of the relatively moderate NO<sub>x</sub>&nbsp;reduction from power plants and the continuing large contribution (over 50% of total NOx emissions) from other&nbsp;sources of NO<sub>x</sub> such as vehicles and nonroad vehicles.<br>• Although visibility has begun to improve in some parts&nbsp;of the U.S., there is still significant impairment of visibility in many national parks and other Class I areas&nbsp;throughout the U.S.<br>• Acid neutralizing capacity is beginning to rise in some&nbsp;surface waters in the Northeast, including lakes in the&nbsp;Adirondack Mountains (see graphic below). This is an&nbsp;indication that recovery from acidification is occurring in&nbsp;those areas.&nbsp;<br data-mce-bogus=\"1\"></p>","language":"English","publisher":"NOAA","usgsCitation":"2005, National Acid Precipitation Assessment Program Report to Congress: An integrated assessment: Report to Congress, 85 p.","productDescription":"85 p.","costCenters":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"links":[{"id":368131,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":368130,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.esrl.noaa.gov/csd/aqrsd/reports/napapreport05.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Burtraw, Dallas","contributorId":219624,"corporation":false,"usgs":false,"family":"Burtraw","given":"Dallas","email":"","affiliations":[],"preferred":false,"id":772705,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Butler, Thomas","contributorId":219625,"corporation":false,"usgs":false,"family":"Butler","given":"Thomas","email":"","affiliations":[],"preferred":false,"id":772706,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Colburn, Kenneth","contributorId":219626,"corporation":false,"usgs":false,"family":"Colburn","given":"Kenneth","email":"","affiliations":[],"preferred":false,"id":772707,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"Driscoll, C.","contributorId":28784,"corporation":false,"usgs":true,"family":"Driscoll","given":"C.","affiliations":[],"preferred":false,"id":772708,"contributorType":{"id":2,"text":"Editors"},"rank":4},{"text":"Grigal, David","contributorId":219627,"corporation":false,"usgs":false,"family":"Grigal","given":"David","email":"","affiliations":[],"preferred":false,"id":772709,"contributorType":{"id":2,"text":"Editors"},"rank":5}]}}
,{"id":72415,"text":"sir20055096 - 2005 - Ground-water movement and nitrate in ground water, East Erda area, Tooele County, Utah, 1997-2000","interactions":[],"lastModifiedDate":"2019-12-30T13:44:33","indexId":"sir20055096","displayToPublicDate":"2005-10-03T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5096","title":"Ground-water movement and nitrate in ground water, East Erda area, Tooele County, Utah, 1997-2000","docAbstract":"Nitrate was discovered in ground water in the east Erda area of Tooele County, Utah, in 1994. The U.S. Geological Survey, in cooperation with Tooele County, investigated the ground-water flow system and water quality in the eastern part of Tooele Valley to determine (1) the vertical and horizontal distribution of nitrate, (2) the direction of movement of the nitrate contamination, and (3) the source of the nitrate. The potentiometric surface of the upper part of the basin-fill aquifer indicates that the general direction of ground-water flow is to the northwest, the flow system is complex, and there is a ground-water mound probably associated with springs. The spatial distribution of nitrate reflects the flow system with the nitrate contamination split into a north and south part by the ground-water mound. The distribution of dissolved solids and sulfate in ground water varies spatially. Vertical profiles of nitrate in water from selected wells indicate that nitrate contamination generally is in the upper part of the saturated zone and in some wells has moved downward. Septic systems, mining and smelting, agriculture, and natural sources were considered to be possible sources of nitrate contamination in the east Erda area. Septic systems are not the source of nitrate because water from wells drilled upgradient of all septic systems in the area had elevated nitrate concentrations. Mining and smelting activity are a possible source of nitrate contamination but few data are available to link nitrate contamination with mining sites. Natural and agricultural sources of nitrate are present east of the Erda area but few data are available about these sources. The source(s) of nitrate in the east Erda area could not be clearly delineated in spite of considerable effort and expenditure of resources.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055096","collaboration":"Prepared in cooperation with Tooele County","usgsCitation":"Susong, D., 2005, Ground-water movement and nitrate in ground water, East Erda area, Tooele County, Utah, 1997-2000 (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5096, 4 sheets: 40.00 x 36.00 inches or smaller, https://doi.org/10.3133/sir20055096.","productDescription":"4 sheets: 40.00 x 36.00 inches or smaller","onlineOnly":"Y","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":334244,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5096/PDF/SIR2005_5096_sheet1.pdf","text":"First part of report","size":"3.5 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,{"id":72385,"text":"ofr20051323 - 2005 - Preliminary integrated geologic map databases for the United States: Alabama, Florida, Georgia, Mississippi, North Carolina, and South Carolina","interactions":[],"lastModifiedDate":"2022-05-11T18:16:22.29721","indexId":"ofr20051323","displayToPublicDate":"2005-10-02T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1323","title":"Preliminary integrated geologic map databases for the United States: Alabama, Florida, Georgia, Mississippi, North Carolina, and South Carolina","docAbstract":"<p class=\"style1\">The growth in the use of Geographic Information Systems (GIS) has highlighted the need for regional and national digital geologic maps attributed with age and lithology information. Such maps can be conveniently used to generate derivative maps for purposes including mineral-resource assessment, metallogenic studies, tectonic studies, and environmental research. This Open-File Report is a preliminary version of part of a series of integrated state geologic map databases that cover the entire United States.</p><p class=\"style1\">The only national-scale digital geologic maps that portray most or all of the United States for the conterminous U.S. are the digital version of the King and Beikman (1974a, b) map at a scale of 1:2,500,000, as digitized by Schruben and others (1994) and the digital version of the Geologic Map of North America (Reed and others, 2005a, b) compiled at a scale of 1:5,000,000 which is currently being prepared by the U.S. Geological Survey. The present series of maps is intended to provide the next step in increased detail. State geologic maps that range in scale from 1:100,000 to 1:1,000,000 are available for most of the country, and digital versions of these state maps are the basis of this product. In a few cases, new digital compilations were prepared (e.g. OH, SC, SD) or existing paper maps were digitized (e.g. KY, TX). For Alaska and Hawaii, new regional maps are being compiled and ultimately new state maps will be produced.</p><p class=\"style1\">The digital geologic maps are presented in standardized formats as ARC/INFO (.e00) export files and as ArcView shape (.shp) files. Accompanying these spatial databases are a set of five supplemental data tables that relate the map units to detailed lithologic and age information. The maps for the CONUS have been fitted to a common set of state boundaries based on the 1:100,000 topographic map series of the United States Geological Survey (USGS). When the individual state maps are merged, the combined attribute tables can be used directly with the merged maps to make derivative maps. No attempt has been made to reconcile differences in mapped geology across state lines.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051323","usgsCitation":"Dicken, C.L., Nicholson, S.W., Horton, J.D., Foose, M.P., and Mueller, J.A., 2005, Preliminary integrated geologic map databases for the United States: Alabama, Florida, Georgia, Mississippi, North Carolina, and South Carolina: U.S. Geological Survey Open-File Report 2005-1323, HTML Document, https://doi.org/10.3133/ofr20051323.","productDescription":"HTML Document","onlineOnly":"Y","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":400524,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73910.htm"},{"id":7387,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1323/","linkFileType":{"id":5,"text":"html"}},{"id":191324,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Alabama, Florida, Georgia, Mississippi, North Carolina, South Carolina","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-87.984916,35.005881],[-84.394903,34.98803],[-83.978286,35.44782],[-82.995803,35.773128],[-82.637165,36.065805],[-82.531292,35.972188],[-82.349957,36.117109],[-82.054142,36.126821],[-81.600934,36.587019],[-75.867044,36.550754],[-75.533012,35.787377],[-75.960069,36.495025],[-75.791637,36.082267],[-76.132005,36.287773],[-76.191715,36.107197],[-76.447812,36.192514],[-76.298733,36.1012],[-76.575936,36.006167],[-76.721445,36.147838],[-76.675462,36.266882],[-76.722996,36.066585],[-76.608052,35.936668],[-76.093697,35.993001],[-76.046813,35.717935],[-75.86042,35.978262],[-75.713502,35.693993],[-76.165392,35.328659],[-76.499251,35.381492],[-76.586349,35.508957],[-76.476706,35.511707],[-76.634468,35.510332],[-76.580187,35.387113],[-77.023912,35.514802],[-76.472273,35.294936],[-76.801426,34.964369],[-76.958465,35.047647],[-76.762931,34.920374],[-76.463468,35.076411],[-76.332044,34.970917],[-76.524712,34.681964],[-76.673619,34.71491],[-76.523303,34.652271],[-76.093349,35.048705],[-76.524199,34.615416],[-76.990262,34.669623],[-77.556943,34.417218],[-77.956881,33.87779],[-78.383964,33.901946],[-78.772737,33.768511],[-79.359961,33.006672],[-79.55756,33.021269],[-79.968468,32.639732],[-80.413487,32.470672],[-80.466342,32.31917],[-80.905378,32.051943],[-80.841913,32.002643],[-81.065255,31.877095],[-81.254218,31.55594],[-81.17831,31.52241],[-81.276862,31.254734],[-81.490586,30.984952],[-81.408484,30.977718],[-81.308978,29.96944],[-80.995423,29.206052],[-80.567361,28.562353],[-80.566432,28.09563],[-80.031362,26.796339],[-80.152896,25.702855],[-80.229107,25.732509],[-80.409103,25.25346],[-80.777499,25.135047],[-81.142278,25.183],[-81.117265,25.354953],[-81.362272,25.824401],[-81.678287,25.845301],[-81.868983,26.378648],[-82.094748,26.48393],[-82.076349,26.958263],[-82.147068,26.789803],[-82.301736,26.841588],[-82.714521,27.500415],[-82.393383,27.837519],[-82.716522,27.958398],[-82.566819,27.858002],[-82.721622,27.663908],[-82.851126,27.8863],[-82.664055,28.606584],[-82.827073,29.158425],[-83.018212,29.151417],[-83.679219,29.918513],[-84.000716,30.096209],[-85.343619,29.672004],[-85.405052,29.938487],[-86.2987,30.363049],[-88.014572,30.222366],[-87.766626,30.262353],[-88.008396,30.684956],[-88.191542,30.317002],[-89.315067,30.375408],[-89.461275,30.174745],[-89.615856,30.223195],[-89.806182,30.567543],[-89.816429,31.002084],[-91.625118,30.999167],[-91.502783,31.595727],[-91.030706,32.114337],[-91.171046,32.176526],[-90.90072,32.330379],[-91.117308,32.495039],[-91.013723,32.598419],[-91.105704,32.590879],[-91.054481,32.722259],[-91.158336,32.822304],[-91.078904,32.951818],[-91.201842,32.961212],[-91.043624,33.274636],[-91.206807,33.433846],[-91.185455,33.653604],[-91.060524,33.77764],[-91.086758,33.95827],[-90.874541,34.072041],[-90.93268,34.214824],[-90.580677,34.410554],[-90.483969,34.877176],[-90.34038,34.860357],[-90.293083,34.974574],[-87.984916,35.005881]]],[[[-81.582923,24.658732],[-81.451267,24.747464],[-81.298028,24.656774],[-81.765993,24.552103],[-81.582923,24.658732]]],[[[-84.777208,29.707398],[-84.696726,29.76993],[-85.036219,29.588919],[-84.777208,29.707398]]],[[[-82.255777,26.703437],[-82.038403,26.456907],[-82.186441,26.489221],[-82.255777,26.703437]]],[[[-80.250581,25.34193],[-80.611693,24.93842],[-80.192336,25.473331],[-80.250581,25.34193]]],[[[-75.753765,35.199612],[-75.523952,35.318198],[-75.533512,35.773577],[-75.52592,35.233839],[-75.982812,35.081513],[-75.753765,35.199612]]]]},\"properties\":{\"name\":\"Alabama\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db6732b8","contributors":{"authors":[{"text":"Dicken, Connie L. 0000-0002-1617-8132 cdicken@usgs.gov","orcid":"https://orcid.org/0000-0002-1617-8132","contributorId":57098,"corporation":false,"usgs":true,"family":"Dicken","given":"Connie","email":"cdicken@usgs.gov","middleInitial":"L.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":285557,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nicholson, Suzanne W. 0000-0002-9365-1894 swnich@usgs.gov","orcid":"https://orcid.org/0000-0002-9365-1894","contributorId":880,"corporation":false,"usgs":true,"family":"Nicholson","given":"Suzanne","email":"swnich@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":285553,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Horton, John D. 0000-0003-2969-9073 jhorton@usgs.gov","orcid":"https://orcid.org/0000-0003-2969-9073","contributorId":1227,"corporation":false,"usgs":true,"family":"Horton","given":"John","email":"jhorton@usgs.gov","middleInitial":"D.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":285554,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Foose, Michael P. mfoose@usgs.gov","contributorId":4756,"corporation":false,"usgs":true,"family":"Foose","given":"Michael","email":"mfoose@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":285555,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mueller, Julia A. L.","contributorId":43861,"corporation":false,"usgs":true,"family":"Mueller","given":"Julia","email":"","middleInitial":"A. L.","affiliations":[],"preferred":false,"id":285556,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":72386,"text":"ofr20051324 - 2005 - Preliminary integrated geologic map databases for the United States: Kentucky, Ohio, Tennessee, and West Virginia","interactions":[],"lastModifiedDate":"2021-12-02T22:43:03.19113","indexId":"ofr20051324","displayToPublicDate":"2005-10-02T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1324","title":"Preliminary integrated geologic map databases for the United States: Kentucky, Ohio, Tennessee, and West Virginia","docAbstract":"<p class=\"style1\">The growth in the use of Geographic Information Systems (GIS) has highlighted the need for regional and national digital geologic maps attributed with age and lithology information. Such maps can be conveniently used to generate derivative maps for purposes including mineral-resource assessment, metallogenic studies, tectonic studies, and environmental research. This Open-File Report is a preliminary version of part of a series of integrated state geologic map databases that cover the entire United States.</p><p class=\"style1\">The only national-scale digital geologic maps that portray most or all of the United States for the conterminous U.S. are the digital version of the King and Beikman (1974a, b) map at a scale of 1:2,500,000, as digitized by Schruben and others (1994) and the generalized digital version (Reed and Bush, 2004) of the Geologic Map of North America (Reed and others, 2005a, b) compiled at a scale of 1:5,000,000. The present series of maps is intended to provide the next step in increased detail. State geologic maps that range in scale from 1:100,000 to 1:1,000,000 are available for most of the country, and digital versions of these state maps are the basis for this product. In a few cases, new digital compilations were prepared (e.g. Ohio, South Carloina, South Dakota) or existing paper maps were digitized (e.g. Kentucky, Texas). Also as part of this series, new regional maps for Alaska and Hawaii are being compiled and ultimately new state maps will be produced.</p><p class=\"style1\">The digital geologic maps are presented in standardized formats as ARC/INFO export (.e00) files and as ArcView shape (.shp) files. Accompanying these spatial databases are a set of five supplemental attribute tables that relate the map units to detailed lithologic and age information. The maps for the CONUS have been fitted to a common set of state boundaries based on the 1:100,000 topographic map series of the United States Geological Survey (USGS). When the individual state maps are merged, the combined attribute tables can be used directly with the merged maps to make derivative maps. No attempt has been made to reconcile differences in mapped geology across state lines.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051324","usgsCitation":"Nicholson, S.W., Dicken, C.L., Horton, J.D., Labay, K., Foose, M.P., and Mueller, J.A., 2005, Preliminary integrated geologic map databases for the United States: Kentucky, Ohio, Tennessee, and West Virginia: U.S. Geological Survey Open-File Report 2005-1324, HTML Document, https://doi.org/10.3133/ofr20051324.","productDescription":"HTML Document","onlineOnly":"Y","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":191325,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":392422,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73911.htm"},{"id":7388,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2005/1324/","text":"Index Page","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Kentucky, Ohio, Tennessee, West Virginia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.3061,\n              34.9864\n            ],\n            [\n              -77.73,\n              34.9864\n            ],\n            [\n              -77.73,\n              41.9778\n            ],\n            [\n              -90.3061,\n              41.9778\n            ],\n            [\n              -90.3061,\n              34.9864\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db67327b","contributors":{"authors":[{"text":"Nicholson, Suzanne W. 0000-0002-9365-1894 swnich@usgs.gov","orcid":"https://orcid.org/0000-0002-9365-1894","contributorId":880,"corporation":false,"usgs":true,"family":"Nicholson","given":"Suzanne","email":"swnich@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":285558,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dicken, Connie L. 0000-0002-1617-8132 cdicken@usgs.gov","orcid":"https://orcid.org/0000-0002-1617-8132","contributorId":57098,"corporation":false,"usgs":true,"family":"Dicken","given":"Connie","email":"cdicken@usgs.gov","middleInitial":"L.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":285562,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Horton, John D. 0000-0003-2969-9073 jhorton@usgs.gov","orcid":"https://orcid.org/0000-0003-2969-9073","contributorId":1227,"corporation":false,"usgs":true,"family":"Horton","given":"John","email":"jhorton@usgs.gov","middleInitial":"D.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":285559,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Labay, Keith A. 0000-0002-6763-3190 klabay@usgs.gov","orcid":"https://orcid.org/0000-0002-6763-3190","contributorId":2097,"corporation":false,"usgs":true,"family":"Labay","given":"Keith A.","email":"klabay@usgs.gov","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":false,"id":285563,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Foose, Michael P. mfoose@usgs.gov","contributorId":4756,"corporation":false,"usgs":true,"family":"Foose","given":"Michael","email":"mfoose@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":285560,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mueller, Julia A. L.","contributorId":43861,"corporation":false,"usgs":true,"family":"Mueller","given":"Julia","email":"","middleInitial":"A. L.","affiliations":[],"preferred":false,"id":285561,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":72387,"text":"ofr20051325 - 2005 - Preliminary integrated geologic map databases for the United States: Delaware, Maryland, New York, Pennsylvania, and Virginia","interactions":[],"lastModifiedDate":"2021-12-02T22:39:35.853082","indexId":"ofr20051325","displayToPublicDate":"2005-10-02T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1325","title":"Preliminary integrated geologic map databases for the United States: Delaware, Maryland, New York, Pennsylvania, and Virginia","docAbstract":"<p class=\"style1\">The growth in the use of Geographic Information Systems (GIS) has highlighted the need for regional and national digital geologic maps attributed with age and lithology information. Such maps can be conveniently used to generate derivative maps for purposes including mineral-resource assessment, metallogenic studies, tectonic studies, and environmental research. This Open-File Report is a preliminary version of part of a series of integrated state geologic map databases that cover the entire United States.</p><p class=\"style1\">The only national-scale digital geologic maps that portray most or all of the United States for the conterminous U.S. are the digital version of the King and Beikman (1974a, b) map at a scale of 1:2,500,000, as digitized by Schruben and others (1994) and the generalized digital version (Reed and Bush, 2004) of the Geologic Map of North America (Reed and others, 2005a, b) compiled at a scale of 1:5,000,000. The present series of maps is intended to provide the next step in increased detail. State geologic maps that range in scale from 1:100,000 to 1:1,000,000 are available for most of the country, and digital versions of these state maps are the basis for this product. In a few cases, new digital compilations were prepared (e.g. Ohio, South Carloina, South Dakota) or existing paper maps were digitized (e.g. Kentucky, Texas). Also as part of this series, new regional maps for Alaska and Hawaii are being compiled and ultimately new state maps will be produced.</p><p class=\"style1\">The digital geologic maps are presented in standardized formats as ARC/INFO export (.e00) files and as ArcView shape (.shp) files. Accompanying these spatial databases are a set of five supplemental attribute tables that relate the map units to detailed lithologic and age information. The maps for the CONUS have been fitted to a common set of state boundaries based on the 1:100,000 topographic map series of the United States Geological Survey (USGS). When the individual state maps are merged, the combined attribute tables can be used directly with the merged maps to make derivative maps. No attempt has been made to reconcile differences in mapped geology across state lines.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051325","usgsCitation":"Dicken, C.L., Nicholson, S.W., Horton, J.D., Kinney, S.A., Gunther, G.L., Foose, M.P., and Mueller, J.A., 2005, Preliminary integrated geologic map databases for the United States: Delaware, Maryland, New York, Pennsylvania, and Virginia: U.S. Geological Survey Open-File Report 2005-1325, HTML Document, https://doi.org/10.3133/ofr20051325.","productDescription":"HTML Document","onlineOnly":"Y","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":191326,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":392420,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73912.htm"},{"id":7389,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2005/1325/","text":"Index Page","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Delaware, Maryland, New York, Pennsylvania, Virginia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.6171875,\n              36.66841891894786\n            ],\n            [\n              -75.41015624999999,\n              36.66841891894786\n            ],\n            [\n              -75.41015624999999,\n              44.213709909702054\n            ],\n            [\n              -82.6171875,\n              44.213709909702054\n            ],\n            [\n              -82.6171875,\n              36.66841891894786\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db6732d0","contributors":{"authors":[{"text":"Dicken, Connie L. 0000-0002-1617-8132 cdicken@usgs.gov","orcid":"https://orcid.org/0000-0002-1617-8132","contributorId":57098,"corporation":false,"usgs":true,"family":"Dicken","given":"Connie","email":"cdicken@usgs.gov","middleInitial":"L.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":285570,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nicholson, Suzanne W. 0000-0002-9365-1894 swnich@usgs.gov","orcid":"https://orcid.org/0000-0002-9365-1894","contributorId":880,"corporation":false,"usgs":true,"family":"Nicholson","given":"Suzanne","email":"swnich@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":285564,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Horton, John D. 0000-0003-2969-9073 jhorton@usgs.gov","orcid":"https://orcid.org/0000-0003-2969-9073","contributorId":1227,"corporation":false,"usgs":true,"family":"Horton","given":"John","email":"jhorton@usgs.gov","middleInitial":"D.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":285565,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kinney, Scott A. 0000-0001-5008-5813 skinney@usgs.gov","orcid":"https://orcid.org/0000-0001-5008-5813","contributorId":1395,"corporation":false,"usgs":true,"family":"Kinney","given":"Scott","email":"skinney@usgs.gov","middleInitial":"A.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":285566,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gunther, Gregory L. 0000-0002-1761-1604 ggunther@usgs.gov","orcid":"https://orcid.org/0000-0002-1761-1604","contributorId":1581,"corporation":false,"usgs":true,"family":"Gunther","given":"Gregory","email":"ggunther@usgs.gov","middleInitial":"L.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true},{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":285567,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Foose, Michael P. mfoose@usgs.gov","contributorId":4756,"corporation":false,"usgs":true,"family":"Foose","given":"Michael","email":"mfoose@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":285568,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Mueller, Julia A. L.","contributorId":43861,"corporation":false,"usgs":true,"family":"Mueller","given":"Julia","email":"","middleInitial":"A. L.","affiliations":[],"preferred":false,"id":285569,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":72362,"text":"sir20055170 - 2005 - Hydrology and simulation of ground-water flow in Cedar Valley, Iron County, Utah","interactions":[],"lastModifiedDate":"2019-12-30T13:58:41","indexId":"sir20055170","displayToPublicDate":"2005-09-27T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5170","title":"Hydrology and simulation of ground-water flow in Cedar Valley, Iron County, Utah","docAbstract":"<p>Cedar Valley, located in the eastern part of Iron County in southwestern Utah, is experiencing rapid population growth. Cedar Valley traditionally has supported agriculture, but the growing population needs a larger share of the available water resources. Water withdrawn from the unconsolidated basin fill is the primary source for public supply and is a major source of water for irrigation. Water managers are concerned about increasing demands on the water supply and need hydrologic information to manage this limited water resource and minimize flow of water unsuitable for domestic use toward present and future public-supply sources.</p><p>Surface water in the study area is derived primarily from snowmelt at higher altitudes east of the study area or from occasional large thunderstorms during the summer. Coal Creek, a perennial stream with an average annual discharge of 24,200 acre-feet per year, is the largest stream in Cedar Valley. Typically, all of the water in Coal Creek is diverted for irrigation during the summer months. All surface water is consumed within the basin by irrigated crops, evapotranspiration, or recharge to the ground-water system.</p><p>Ground water in Cedar Valley generally moves from primary recharge areas along the eastern margin of the basin where Coal Creek enters, to areas of discharge or subsurface outflow. Recharge to the unconsolidated basin-fill aquifer is by seepage of unconsumed irrigation water, streams, direct precipitation on the unconsolidated basin fill, and subsurface inflow from consolidated rock and Parowan Valley and is estimated to be about 42,000 acre-feet per year. Stable-isotope data indicate that recharge is primarily from winter precipitation. The chloride mass-balance method indicates that recharge may be less than 42,000 acre-feet per year, but is considered a rough approximation because of limited chloride concentration data for precipitation and Coal Creek. Continued declining water levels indicate that recharge is not sufficient to meet demand. Water levels in many areas are at or close to historic lows.</p><p>In 2000, withdrawal from wells was estimated to be 36,000 acre-feet per year. About 4,000 acre-feet per year are estimated to discharge to evapotranspiration or as subsurface outflow. Prior to large-scale ground-water development, ground-water discharge by evapotranspiration and discharge to springs was much larger.</p><p>Ground water along the eastern margin of the valley between Cedar City and Enoch is unsuitable for domestic use because of high dissolved-solids and nitrate concentrations. The predominant ions of Ca and SO4 in this area indicate dissolution of gypsum in the Markagunt Plateau to the east. Data collected during this study were compared to historic data; there is no evidence to indicate deterioration in ground-water quality. The spatial distribution of ground water with high nitrate concentration does not appear to be migrating beyond its previously known extent. <br>No single source can be identified as the cause for elevated nitrate concentrations in ground water. Low nitrogen-15 values north of Cedar City indicate a natural geologic source. Higher nitrogen-15 values toward the center of the basin and associated hydrologic data indicate probable recharge from waste-water effluent. Excess dissolved nitrogen gas and low nitrate concentrations in shallow ground water indicate that denitrification is occurring in some areas.</p><p>A computer ground-water flow model was developed to simulate flow in the unconsolidated basin fill. The method of determining recharge from irrigation was changed during the calibration process to incorporate more areal and temporal variability. In general, the model accurately simulates water levels and water-level fluctuations and can be considered an adequate tool to help determine the valley-wide effects on water levels of additional ground-water withdrawals and changes in water use. The model was used to simulated water-level changes caused by projecting current withdrawal rates, increased withdrawal rates, and a 10-year drought. Water levels declined 20 to 275 feet in the southern and central parts of the valley and less than 20 feet north of Enoch</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/sir20055170","collaboration":"Prepared in cooperation with the Central Iron County Water Conservancy District; Utah Department of Natural Resources, Division of Water Resources; Utah Department of Environmental Quality, Division of Water Quality; Cedar City, and City of Enoch","usgsCitation":"Brooks, L.E., and Mason, J.L., 2005, Hydrology and simulation of ground-water flow in Cedar Valley, Iron County, Utah (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5170, x, 114 p., https://doi.org/10.3133/sir20055170.","productDescription":"x, 114 p.","numberOfPages":"127","onlineOnly":"Y","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":193036,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7325,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5170/","linkFileType":{"id":5,"text":"html"}},{"id":334242,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5170/PDF/SIR2005_5170.pdf"}],"country":"United States","state":"Utah","county":"Iron County","otherGeospatial":"Cedar Valley","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-112.4806,38.1474],[-112.4806,38.1379],[-112.4805,38.1293],[-112.481,38.1148],[-112.481,38.1098],[-112.4808,38.0862],[-112.4813,38.0658],[-112.4818,38.0572],[-112.4817,38.0418],[-112.4822,38.0273],[-112.4825,37.9847],[-112.483,37.9788],[-112.4696,37.9789],[-112.4707,37.9635],[-112.4706,37.9462],[-112.4711,37.9349],[-112.4715,37.9059],[-112.489,37.9063],[-112.4895,37.8913],[-112.5075,37.8912],[-112.5245,37.8912],[-112.5256,37.8912],[-112.5623,37.8905],[-112.5909,37.8909],[-112.5909,37.8832],[-112.5815,37.8832],[-112.5812,37.8383],[-112.5815,37.8057],[-112.5949,37.8065],[-112.6275,37.8082],[-112.6491,37.8085],[-112.6567,37.8076],[-112.6928,37.8065],[-112.6931,37.7752],[-112.6934,37.7525],[-112.6931,37.7185],[-112.6902,37.7186],[-112.6877,37.574],[-112.6874,37.545],[-112.7641,37.5445],[-112.7948,37.5448],[-112.8331,37.5449],[-112.8534,37.5448],[-112.9051,37.5449],[-112.9047,37.5154],[-112.9046,37.5005],[-112.9452,37.5006],[-113.0415,37.5007],[-113.0411,37.4744],[-113.0817,37.4745],[-113.1496,37.4748],[-113.1497,37.4803],[-113.2024,37.4807],[-113.2123,37.4806],[-113.2175,37.4805],[-113.2605,37.481],[-113.2601,37.4946],[-113.2604,37.5114],[-113.2601,37.5313],[-113.2775,37.5311],[-113.2955,37.5314],[-113.3153,37.5307],[-113.4772,37.5302],[-113.4779,37.5946],[-113.4784,37.6182],[-113.5144,37.6186],[-113.5324,37.6189],[-113.5353,37.6188],[-113.5539,37.619],[-113.5917,37.619],[-113.592,37.6059],[-113.61,37.6061],[-113.7204,37.6068],[-113.7402,37.6065],[-113.7564,37.6068],[-113.7599,37.6067],[-113.7936,37.6067],[-113.8128,37.6073],[-113.8686,37.6074],[-113.8872,37.6071],[-113.904,37.6068],[-113.9232,37.607],[-114.0539,37.6075],[-114.0541,37.6431],[-114.0541,37.6447],[-114.0539,37.666],[-114.0536,37.7109],[-114.0535,37.7259],[-114.0531,37.7887],[-114.0531,37.7903],[-114.0524,37.9039],[-114.0524,37.9059],[-114.0494,38.0308],[-114.0494,38.0329],[-114.0493,38.1503],[-114.0445,38.1499],[-114.0246,38.1502],[-114.0077,38.1505],[-113.9889,38.1504],[-113.955,38.1505],[-113.9368,38.1503],[-113.9333,38.1508],[-113.9164,38.1506],[-113.8988,38.1509],[-113.8807,38.1507],[-113.8438,38.1508],[-113.8239,38.1507],[-113.8069,38.1505],[-113.787,38.1508],[-113.7688,38.1506],[-113.7343,38.1506],[-113.7144,38.1504],[-113.6957,38.1507],[-113.6781,38.1509],[-113.6594,38.1507],[-113.643,38.151],[-113.6225,38.1508],[-113.605,38.151],[-113.5862,38.1508],[-113.5657,38.1506],[-113.5546,38.1508],[-113.547,38.1504],[-113.5142,38.1508],[-113.4961,38.1506],[-113.4926,38.1506],[-113.4738,38.1504],[-113.4545,38.1506],[-113.4364,38.1504],[-113.4042,38.1498],[-113.3814,38.1501],[-113.3638,38.1498],[-113.3474,38.1496],[-113.3351,38.1497],[-113.3111,38.1495],[-113.2924,38.1488],[-113.2736,38.149],[-113.2034,38.1493],[-113.1999,38.1493],[-113.1812,38.149],[-113.163,38.1488],[-113.1449,38.1485],[-113.1267,38.1491],[-113.108,38.1488],[-113.0717,38.1482],[-113.0536,38.1484],[-113.0325,38.1481],[-113.012,38.1483],[-112.9939,38.1484],[-112.9605,38.1482],[-112.9418,38.1484],[-112.9383,38.1484],[-112.9202,38.1485],[-112.9014,38.1487],[-112.8833,38.1484],[-112.8499,38.1491],[-112.8318,38.1487],[-112.8277,38.1488],[-112.8101,38.1489],[-112.7902,38.149],[-112.7715,38.1487],[-112.7381,38.1489],[-112.7194,38.1481],[-112.7165,38.1485],[-112.6989,38.1482],[-112.6773,38.1483],[-112.6585,38.1484],[-112.6275,38.1486],[-112.6094,38.1491],[-112.6035,38.1492],[-112.5854,38.1488],[-112.5673,38.1489],[-112.5485,38.1485],[-112.5356,38.1486],[-112.5304,38.1481],[-112.5134,38.1478],[-112.4806,38.1474]]]},\"properties\":{\"name\":\"Iron\",\"state\":\"UT\"}}]}","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e865","contributors":{"authors":[{"text":"Brooks, Lynette E. 0000-0002-9074-0939 lebrooks@usgs.gov","orcid":"https://orcid.org/0000-0002-9074-0939","contributorId":2718,"corporation":false,"usgs":true,"family":"Brooks","given":"Lynette","email":"lebrooks@usgs.gov","middleInitial":"E.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285487,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mason, James L.","contributorId":14397,"corporation":false,"usgs":true,"family":"Mason","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":285488,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72254,"text":"ofr20051006_2005 - 2005 - Potentiometric surface map of the Magothy aquifer in southern Maryland, September, 2003","interactions":[],"lastModifiedDate":"2023-03-09T20:49:22.817505","indexId":"ofr20051006_2005","displayToPublicDate":"2005-09-19T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1006","title":"Potentiometric surface map of the Magothy aquifer in southern Maryland, September, 2003","docAbstract":"This report presents a map showing the potentiometric surface of the Magothy aquifer in the Magothy Formation of Upper Cretaceous age in Southern Maryland during September 2002. The map is based on water-level measurements in 79 wells. The highest measured water level was 83 feet above sea level near the northern boundary and outcrop area of the aquifer in the north-central part of Anne Arundel County.\r\n\r\nThe potentiometric surface declined towards the south and east. Local gradients were directed toward the centers of two cones of depression that developed in response to pumping. These cones of depression were centered around well fields in the Waldorf area and at the Chalk Point power plant. Measured ground-water levels were as low as 81 feet below sea level in the Waldorf area and 75 feet below sea level at Chalk Point.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051006_2005","usgsCitation":"Curtin, S.E., Andreasen, D., and Wheeler, J.C., 2005, Potentiometric surface map of the Magothy aquifer in southern Maryland, September, 2003: U.S. Geological Survey Open-File Report 2005-1006, 1 p., https://doi.org/10.3133/ofr20051006_2005.","productDescription":"1 p.","temporalStart":"2003-09-01","temporalEnd":"2003-09-30","costCenters":[{"id":41514,"text":"Maryland-Delaware-District of Columbia  Water Science Center","active":true,"usgs":true}],"links":[{"id":191623,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8906,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1006/","linkFileType":{"id":5,"text":"html"}},{"id":409012,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_78439.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Maryland","otherGeospatial":"Magothy aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -77.0667,\n              38.26667\n            ],\n            [\n              -76,\n              38.2667\n            ],\n            [\n              -76,\n              39.2197\n            ],\n            [\n              -77.0667,\n              39.2197\n            ],\n            [\n              -77.0667,\n              38.2667\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db68310d","contributors":{"authors":[{"text":"Curtin, Stephen E. securtin@usgs.gov","contributorId":3703,"corporation":false,"usgs":true,"family":"Curtin","given":"Stephen","email":"securtin@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285271,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreasen, David C.","contributorId":59003,"corporation":false,"usgs":true,"family":"Andreasen","given":"David C.","affiliations":[],"preferred":false,"id":285273,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wheeler, Judith C.","contributorId":13620,"corporation":false,"usgs":true,"family":"Wheeler","given":"Judith","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":285272,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72233,"text":"sir20055141 - 2005 - Ground-water modeling of pumping effects near regional ground-water divides and river/aquifer systems - Results and implications of numerical experiments","interactions":[],"lastModifiedDate":"2012-02-02T00:14:02","indexId":"sir20055141","displayToPublicDate":"2005-09-16T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5141","title":"Ground-water modeling of pumping effects near regional ground-water divides and river/aquifer systems - Results and implications of numerical experiments","docAbstract":"Agreements between United States governors and Canadian territorial premiers establish water-management principles and a framework for protecting Great Lakes waters, including ground water, from diversion and consumptive uses. The issue of ground-water diversions out of the Great Lakes Basin by large-scale pumping near the divides has been raised. Two scenario models, in which regional ground-water flow models represent major aquifers in the Great Lakes region, were used to assess the effect of pumping near ground-water divides. The regional carbonate aquifer model was a generalized model representing northwestern Ohio and northeastern Indiana; the regional sandstone aquifer model used an existing calibrated ground-water flow model for southeastern Wisconsin. Various well locations and pumping rates were examined. Although the two models have different frameworks and boundary conditions, results of the models were similar. There was significant diversion of ground water across ground-water divides due to pumping within 10 miles of the divides. In the regional carbonate aquifer model, the percentage of pumped water crossing the divide ranges from about 20 percent for a well 10 miles from the divide to about 50 percent for a well adjacent to the divide. In the regional sandstone aquifer model, the percentages range from about 30 percent for a well 10 miles from the divide to about 50 percent for a well adjacent to the divide; when pumping on the west side of the divide, within 5 mi of the predevelopment divide, results in at least 10 percent of the water being diverted from the east side of the divide. Two additional scenario models were done to examine the effects of pumping near rivers. Transient models were used to simulate a rapid stage rise in a river during pumping at a well in carbonate and glacial aquifers near the river. Results of water-budget analyses indicate that induced infiltration, captured streamflow, and underflow were important for both glacial and carbonate aquifers; however, in many cases, traveltimes from the river to the well will limit river water from physically entering the well.","language":"ENGLISH","doi":"10.3133/sir20055141","usgsCitation":"Sheets, R., Dumouchelle, D.H., and Feinstein, D.T., 2005, Ground-water modeling of pumping effects near regional ground-water divides and river/aquifer systems - Results and implications of numerical experiments: U.S. Geological Survey Scientific Investigations Report 2005-5141, v, 31 p. : ill., https://doi.org/10.3133/sir20055141.","productDescription":"v, 31 p. : ill.","costCenters":[],"links":[{"id":192829,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7056,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5141/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db6608b9","contributors":{"authors":[{"text":"Sheets, Rodney A. rasheets@usgs.gov","contributorId":1848,"corporation":false,"usgs":true,"family":"Sheets","given":"Rodney A.","email":"rasheets@usgs.gov","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285218,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dumouchelle, Denise H. ddumouch@usgs.gov","contributorId":1847,"corporation":false,"usgs":true,"family":"Dumouchelle","given":"Denise","email":"ddumouch@usgs.gov","middleInitial":"H.","affiliations":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285217,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Feinstein, Daniel T. 0000-0003-1151-2530 dtfeinst@usgs.gov","orcid":"https://orcid.org/0000-0003-1151-2530","contributorId":1907,"corporation":false,"usgs":true,"family":"Feinstein","given":"Daniel","email":"dtfeinst@usgs.gov","middleInitial":"T.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285219,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":71919,"text":"ofr20051217 - 2005 - Undiscovered oil resources in the Federal portion of the 1002 Area of the Arctic National Wildlife Refuge: An economic update","interactions":[],"lastModifiedDate":"2022-09-12T13:38:54.445079","indexId":"ofr20051217","displayToPublicDate":"2005-09-07T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1217","title":"Undiscovered oil resources in the Federal portion of the 1002 Area of the Arctic National Wildlife Refuge: An economic update","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051217","usgsCitation":"Attanasi, E., 2005, Undiscovered oil resources in the Federal portion of the 1002 Area of the Arctic National Wildlife Refuge: An economic update (Version 1.0): U.S. Geological Survey Open-File Report 2005-1217, iv, 29 p., https://doi.org/10.3133/ofr20051217.","productDescription":"iv, 29 p.","onlineOnly":"Y","costCenters":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":191062,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":406475,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73652.htm","linkFileType":{"id":5,"text":"html"}},{"id":7437,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1217/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","otherGeospatial":"1002 Area, Arctic National Wildlife Refuge","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -146.4667,\n              69.5667\n            ],\n            [\n              -142.1,\n              69.5667\n            ],\n            [\n              -142.1,\n              70.1667\n            ],\n            [\n              -146.4667,\n              70.1667\n            ],\n            [\n              -146.4667,\n              69.5667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f60f","contributors":{"authors":[{"text":"Attanasi, Emil D. 0000-0001-6845-7160 attanasi@usgs.gov","orcid":"https://orcid.org/0000-0001-6845-7160","contributorId":198728,"corporation":false,"usgs":true,"family":"Attanasi","given":"Emil D.","email":"attanasi@usgs.gov","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":284888,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71118,"text":"sir20055113 - 2005 - Water budgets for selected watersheds in the Delaware River basin, eastern Pennsylvania and western New Jersey","interactions":[],"lastModifiedDate":"2017-06-09T10:22:52","indexId":"sir20055113","displayToPublicDate":"2005-08-30T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5113","title":"Water budgets for selected watersheds in the Delaware River basin, eastern Pennsylvania and western New Jersey","docAbstract":"This pilot study, done by the U.S. Geological Survey in cooperation with the Delaware River Basin Commission, developed annual water budgets using available data for five watersheds in the Delaware River Basin with different degrees of urbanization and different geological settings. A basin water budget and a water-use budget were developed for each watershed. The basin water budget describes inputs to the watershed (precipitation and imported water), outputs of water from the watershed (streamflow, exported water, leakage, consumed water, and evapotranspiration), and changes in ground-water and surface-water storage. The water-use budget describes water withdrawals in the watershed (ground-water and surface-water withdrawals), discharges of water in the watershed (discharge to surface water and ground water), and movement of water of water into and out of the watershed (imports, exports, and consumed water). The water-budget equations developed for this study can be applied to any watershed in the Delaware River Basin. Data used to develop the water budgets were obtained from available long-term meteorological and hydrological data-collection stations and from water-use data collected by regulatory agencies. In the Coastal Plain watersheds, net ground-water loss from unconfined to confined aquifers was determined by using ground-water-flow-model simulations. Error in the water-budget terms is caused by missing data, poor or incomplete measurements, overestimated or underestimated quantities, measurement or reporting errors, and the use of point measurements, such as precipitation and water levels, to estimate an areal quantity, particularly if the watershed is hydrologically or geologically complex or the data-collection station is outside the watershed. The complexity of the water budgets increases with increasing watershed urbanization and interbasin transfer of water. In the Wissahickon Creek watershed, for example, some ground water is discharged to streams in the watershed, some is exported as wastewater, and some is exported for public supply. In addition, ground water withdrawn outside the watershed is imported for public supply or imported as wastewater for treatment and discharge in the watershed. A GIS analysis was necessary to quantify many of the water-budget components. \r\n\r\nThe 89.9-square mile East Branch Brandywine Creek watershed in Pennsylvania is a rural watershed with reservoir storage that is underlain by fractured rock. Water budgets were developed for 1977-2001. Average annual precipitation, streamflow, and evapotranspiration were 46.89, 21.58, and 25.88 inches, respectively. Some water was imported (average of 0.68 inches) into the watershed for public-water supply and as wastewater for treatment and discharge; these imports resulted in a net gain of water to the watershed. More water was discharged to East Branch Brandywine Creek than was withdrawn from it; the net discharge resulted in an increase in streamflow. Most ground water was withdrawn (average of 0.25 inches) for public-water supply. Surface water was withdrawn (average of 0.58 inches) for public-water and industrial supply. Discharge of water by sewage-treatment plants and industries (average of 1.22 inches) and regulation by Marsh Creek Reservoir caused base flow to appear an average of 7.2 percent higher than it would have been without these additional sources. On average, 67 percent of the difference was caused by sewage-treatment-plant and industrial discharges, and 33 percent was caused by regulation of the Marsh Creek Reservoir. Water imports, withdrawals, and discharges have been increasing as the watershed becomes increasingly urbanized. \r\n\r\nThe 64-square mile Wissahickon Creek watershed in Pennsylvania is an urban watershed underlain by fractured rock. Water budgets were developed for 1987-98. Average annual precipitation, streamflow, and evapotranspiration were 47.23, 22.24, and 23.12 inches, respectively. The watershed is highly u","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055113","usgsCitation":"Sloto, R.A., and Buxton, D.E., 2005, Water budgets for selected watersheds in the Delaware River basin, eastern Pennsylvania and western New Jersey: U.S. Geological Survey Scientific Investigations Report 2005-5113, 45 p., https://doi.org/10.3133/sir20055113.","productDescription":"45 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":6821,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5113/","linkFileType":{"id":5,"text":"html"}},{"id":192649,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Pennsylvania","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77,38.833333333333336 ], [ -77,42.833333333333336 ], [ -74,42.833333333333336 ], [ -74,38.833333333333336 ], [ -77,38.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478ee4b07f02db489ec1","contributors":{"authors":[{"text":"Sloto, Ronald A. rasloto@usgs.gov","contributorId":424,"corporation":false,"usgs":true,"family":"Sloto","given":"Ronald","email":"rasloto@usgs.gov","middleInitial":"A.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":283683,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buxton, Debra E. dbuxton@usgs.gov","contributorId":4777,"corporation":false,"usgs":true,"family":"Buxton","given":"Debra","email":"dbuxton@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":283684,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71121,"text":"sir20055181 - 2005 - Hydrologic conditions and lake-level fluctuations at Long Lost Lake, 1939-2004, White Earth Indian Reservation, Clearwater County, Minnesota","interactions":[],"lastModifiedDate":"2016-04-04T08:17:30","indexId":"sir20055181","displayToPublicDate":"2005-08-30T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5181","title":"Hydrologic conditions and lake-level fluctuations at Long Lost Lake, 1939-2004, White Earth Indian Reservation, Clearwater County, Minnesota","docAbstract":"<p>Long Lost Lake, a closed-basin lake in Clearwater County, Minnesota, has had a substantial rise in lake level since 1990. The increased level and surface area of the lake has led to the inundation of nearby homes and roads. The U.S. Geological Survey, in cooperation with the White Earth Band of Chippewa Indians, conducted a study to document the historical lake-level fluctuations, to investigate reasons for hydrologic change, and to develop a general understanding of the hydrology of lakes that have had rapid changes in lake level.</p>\n<p>Lake levels were recorded continuously from August 2003 through December 2004. The purpose was to establish a temporal, detailed record of lake levels and to connect this record to precipitation and ground-water-level data. A long-term record is critical to understanding the relation between surface water and ground water. This is especially true for closed-basin lakes. Between August 2003 and December 2004, the lake level generally declined. The highest lake altitude was 492.58 meters above NAVD 88 on August 5, 2003, and the low of 492.11 meters above NAVD 88 occurred on August 29, 2004.</p>\n<p>Results of water-level measurements in 5 observation wells and 14 wetlands and ponds show that the water-table level is substantially higher on the north side of the lake than the lake level, providing the head pressure necessary for ground-water discharge into Long Lost Lake. In contrast, on the south and east sides of the lake, water-table levels are similar to the lake level. This indicates a general north-northwest to south-southeast ground-water flow direction. Results of a synoptic survey of lake temperature and other measurements supported the direction of water inflow and outflow.</p>\n<p>Aerial photography and a geographic information system were used to construct a historical lake record from 1939 to 2001. Lake-level increases match similar increases in precipitation, indicating a strong link between the two. Results show that lake-level increases in Long Lost Lake appear to primarily be due to natural rather than anthropogenic effects.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055181","collaboration":"Prepared in cooperation with the White Earth Band of Chippewa Indians","usgsCitation":"Christensen, V.G., and Bergman, A.L., 2005, Hydrologic conditions and lake-level fluctuations at Long Lost Lake, 1939-2004, White Earth Indian Reservation, Clearwater County, Minnesota: U.S. Geological Survey Scientific Investigations Report 2005-5181, v, 18 p., https://doi.org/10.3133/sir20055181.","productDescription":"v, 18 p.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":319745,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20055181.JPG"},{"id":6822,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5181/","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","country":"United States","state":"Minnesota","otherGeospatial":"Long Lost Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.41128158569335,\n              47.21572047609892\n            ],\n            [\n              -95.40836334228516,\n              47.21676985912015\n            ],\n            [\n              -95.40647506713867,\n              47.219451521380755\n            ],\n            [\n              -95.40184020996094,\n              47.2186353776589\n            ],\n            [\n              -95.39857864379883,\n              47.216886455951716\n            ],\n            [\n              -95.39634704589844,\n              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vglenn@usgs.gov","orcid":"https://orcid.org/0000-0003-4166-7461","contributorId":2354,"corporation":false,"usgs":true,"family":"Christensen","given":"Victoria","email":"vglenn@usgs.gov","middleInitial":"G.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":283685,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bergman, Andrea L.","contributorId":10683,"corporation":false,"usgs":true,"family":"Bergman","given":"Andrea","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":283686,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71057,"text":"wri034125 - 2005 - Borehole-geophysical and hydraulic investigation of the fractured-rock aquifer near the University of Connecticut Landfill, Storrs, Connecticut, 2000 to 2001","interactions":[],"lastModifiedDate":"2019-10-17T07:20:04","indexId":"wri034125","displayToPublicDate":"2005-08-22T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2003-4125","displayTitle":"Borehole-Geophysical and Hydraulic Investigation of the Fractured-Rock Aquifer near the University of Connecticut Landfill, Storrs, Connecticut, 2000 to 2001","title":"Borehole-geophysical and hydraulic investigation of the fractured-rock aquifer near the University of Connecticut Landfill, Storrs, Connecticut, 2000 to 2001","docAbstract":"<p>An integrated borehole-geophysical and hydraulic investigation was conducted at the former landfill area near the University of Connecticut in Storrs, Connecticut, where solvents and landfill leachate have contaminated a fractured-bedrock aquifer. Borehole-geophysical techniques and hydraulic methods were used to characterize the site bedrock lithology and structure, fractures, and hydraulic properties. The geophysical and hydraulic methods included conventional logs, borehole imaging, borehole radar, flowmeter under ambient- and stressed hydraulic conditions, and discrete-zone hydraulic testing, sampling, and monitoring. </p><p>The conventional geophysical-logging methods included caliper, deviation, electromagnetic induction, gamma, specific conductance, and fluid temperature. The advanced methods included optical and acoustic imaging of the borehole wall, heat-pulse flowmeter, and directional radar reflection. </p><p>Borehole-geophysical methods were used to further define conductive features identified with surface-geophysical methods in the first phase of the investigation. The results of the surface- and borehole-geophysical logging were evaluated in an iterative and integrated manner to develop a conceptual model of ground-water flow at the site. </p><p>The rock type, foliation, and fractures at the site were characterized from high-resolution optical televiewer (OTV) images of rocks penetrated by the boreholes and were compared to drilling logs and conventional geophysical logs. The rocks are interpreted as fine- to mediumgrained quartz-feldspar-biotite-garnet gneiss and schist with local intrusions of quartz diorite and pegmatite and minor concentrations of sulfide mineralization similar to rocks described as the Bigelow Brook Formation on regional geologic maps. Layers containing high concentrations of sulfide minerals appear as high electrical conductivity zones on electromagnetic-induction and borehole-radar logs. Foliation in the rocks generally strikes to the southwest and northeast, and dips to the northwest and southeast consistent with previous investigations in this area. The orientation of foliation, however, varies locally and with depth in some of the boreholes. These results are consistent with geologic mapping that has identified small-scale folding. </p><p>The orientations of the transmissive fractures identified in the six boreholes logged for this investigation are similar to the fracture orientations mapped in a previous investigation. Many of these fractures are oriented with a north-northwest strike and have a shallow dip to the west. Other transmissive fractures have a southwest strike and dip at shallow angles to the northwest, and some strike roughly east-west and dip to the north and south. </p><p>Flowmeter logging was used to identify transmissive fractures and to estimate the hydraulic properties in the boreholes. Ambient down flow was measured in one borehole, and ambient up flow and down flow were measured in another borehole. The other four bedrock boreholes did not have measurable vertical flow. Under low-rate pumping conditions (0.25 to 0.5 gallons per minute), one to three inflow zones were identified in each well. Commonly, fractures that are active under ambient conditions contribute to the well under pumping conditions. The ambient conditions were incorporated into the determination of the relative proportions of transmissivity. </p><p>Specific capacity and transmissivity were determined for these open-hole low-rate pumping tests. Quasi-steady-state water levels were reached in four of the boreholes, including MW201R, MW204R, MW302R, and W202-NE. When pumped at low-rate conditions for 0.5 to 4 hours, the specific capacity ranged from 0.03 to 0.18 gallons per minute per foot. The open-hole transmissivity estimates ranged from 4.9 to 30 feet squared per day (ft2/d). </p><p>Open-hole transmissivity was determined for boreholes that did not reach quasi-steady-state conditions under low-rate pumping conditions. Transmissivity was estimated for MW201R, MW202R, and MW203R using non-equilibrium methods, pumping rate, and the transient drawdown data to estimate the open-hole transmissivity. Transmissivity in these boreholes ranged from 0.98 to 3.2 ft<sup>2</sup>/d. </p><p>The transmissivity and head of individual fractures or zones of fractures were estimated from heat-pulse flowmeter data acquired under ambient and stressed conditions. In the absence of ambient flow, data from two profiles of heat-pulse flowmeter data under two different stressed conditions were used to estimate the transmissivity and head of individual fracture zones. Only two boreholes, MW302R and W202-NE, had sufficient data for these analyses. The estimated transmissivity of individual transmissive zones ranged from 1.2 to 9.2 ft<sup>2</sup>/d. The transmissivity values determined by this numerical simulation method were less than the open-hole estimations, which were 15 and 30 ft<sup>2</sup>/d. </p><p>Transmissivity also was measured directly over discrete intervals of the borehole using a straddle-packer apparatus and constant-rate pumping tests. Pumping rates were less than or equal to 0.25 gallons per minute. These discretezone single-hole pumping tests were conducted over a short period of time, usually about 30 minutes to 1 hour in duration. Pumping continued until the test zone reached a steady-state water level or until it was determined that the zone could not yield water at the pumped rate. The estimated transmissivity of individual transmissive zones ranged from about 0.21 to 11 ft<sup>2</sup>/d. The zone at a depth of 197 feet in W202-NE was the only zone that had discrete-interval testing with a straddle packer and sufficient heat-pulse flowmeter data for modeling the flow and estimating transmissivity and head. The two methods produced similar results. The straddle-packer method estimated a transmissivity of 4.7 ft<sup>2</sup>/d, and the heat-pulse flowmeter modeling results estimated a transmissivity of 6.9 ft<sup>2</sup>/d. </p><p>A comparison of the transmissivity estimates indicate estimates typically are within an order of magnitude. The heat-pulse flowmeter methods used in this investigation to determine transmissivity of the boreholes and the individual fractures measure only the upper two or three orders of magnitude of transmissivity. Hence, other fractures in these boreholes permit the movement of water; their transmissivities, however, are lower than the detection limits of the methods that were used for this investigation and very small compared to the transmissive fractures that were studied. </p><p>The data collected in this investigation were used to design discrete-zone monitoring systems for four of the boreholes used for monitoring. The results of the investigation are useful for refining the conceptual site model of ground-water flow, and for providing critical information for interpreting the results of water-quality sampling.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri034125","usgsCitation":"Johnson, C.D., Joesten, P.K., and Mondazzi, R.A., 2005, Borehole-geophysical and hydraulic investigation of the fractured-rock aquifer near the University of Connecticut Landfill, Storrs, Connecticut, 2000 to 2001: U.S. Geological Survey Water-Resources Investigations Report 2003-4125, vi, 133 p., https://doi.org/10.3133/wri034125.","productDescription":"vi, 133 p.","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"links":[{"id":101514,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2003/4125/report.pdf","size":"24559","linkFileType":{"id":1,"text":"pdf"}},{"id":185466,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2003/4125/report-thumb.jpg"}],"country":"United States","state":"Connecticut","city":"Storrs","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72.27075934410095,\n              41.807708943063126\n            ],\n            [\n              -72.26415038108826,\n              41.807708943063126\n            ],\n            [\n              -72.26415038108826,\n              41.811227582554736\n            ],\n            [\n              -72.27075934410095,\n              41.811227582554736\n            ],\n            [\n              -72.27075934410095,\n              41.807708943063126\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6029c7","contributors":{"authors":[{"text":"Johnson, Carole D. 0000-0001-6941-1578 cjohnson@usgs.gov","orcid":"https://orcid.org/0000-0001-6941-1578","contributorId":1891,"corporation":false,"usgs":true,"family":"Johnson","given":"Carole","email":"cjohnson@usgs.gov","middleInitial":"D.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":283571,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Joesten, Peter K. pjoesten@usgs.gov","contributorId":1929,"corporation":false,"usgs":true,"family":"Joesten","given":"Peter","email":"pjoesten@usgs.gov","middleInitial":"K.","affiliations":[{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true},{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":283572,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mondazzi, Remo A.","contributorId":77898,"corporation":false,"usgs":true,"family":"Mondazzi","given":"Remo","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":283573,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":71059,"text":"cir1278 - 2005 - Water withdrawals and trends from the Floridan aquifer system in the southeastern United States, 1950-2000","interactions":[],"lastModifiedDate":"2012-02-02T00:13:49","indexId":"cir1278","displayToPublicDate":"2005-08-22T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1278","title":"Water withdrawals and trends from the Floridan aquifer system in the southeastern United States, 1950-2000","docAbstract":"The Floridan aquifer system in the southeastern United States is one of the most productive aquifers in the world (Miller, 1990). This aquifer system underlies an area of about 100,000 square miles in southern Alabama, eastern and southern Georgia, southeastern Mississippi, southern South Carolina, and all of Florida. The Floridan aquifer system is the primary source of water for nearly 10 million people and supports agriculture, industry, and tourism throughout most of the region. In most areas, water from this aquifer is potable and needs very little treatment before use. However, in southern Florida (south of Lake Okeechobee), northwestern Florida and southern Alabama and Mississippi (Pensacola and westward), and eastern South Carolina, water in the aquifer system generally is not potable.\r\n\r\nThe purpose of this report is to: \r\n\r\nProvide a general description of the Floridan aquifer system; \r\n\r\nDiscuss water withdrawals by category for 2000; \r\n\r\nHighlight trends in water withdrawals between 1950 and 2000; and \r\n\r\nProvide a brief summary on the effects that human impacts have on the Floridan aquifer system. \r\n\r\n","language":"ENGLISH","doi":"10.3133/cir1278","usgsCitation":"Marella, R.L., and Berndt, M., 2005, Water withdrawals and trends from the Floridan aquifer system in the southeastern United States, 1950-2000: U.S. Geological Survey Circular 1278, 24 p., https://doi.org/10.3133/cir1278.","productDescription":"24 p.","costCenters":[],"links":[{"id":185468,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6728,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/circ/2005/1278/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd127","contributors":{"authors":[{"text":"Marella, Richard L. 0000-0003-4861-9841 rmarella@usgs.gov","orcid":"https://orcid.org/0000-0003-4861-9841","contributorId":2443,"corporation":false,"usgs":true,"family":"Marella","given":"Richard","email":"rmarella@usgs.gov","middleInitial":"L.","affiliations":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true},{"id":5051,"text":"FLWSC-Orlando","active":true,"usgs":true}],"preferred":true,"id":283580,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berndt, Marian P.","contributorId":45296,"corporation":false,"usgs":true,"family":"Berndt","given":"Marian P.","affiliations":[],"preferred":false,"id":283581,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72278,"text":"fs20053054 - 2005 - Negative effects of commercial mussel dragging on eelgrass beds in Maine","interactions":[],"lastModifiedDate":"2024-06-21T16:32:27.261445","indexId":"fs20053054","displayToPublicDate":"2005-08-20T09:40:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-3054","displayTitle":"Negative Effects of Commercial Mussel Dragging on Eelgrass Beds in Maine","title":"Negative effects of commercial mussel dragging on eelgrass beds in Maine","docAbstract":"<div><div class=\"abstract-contents\">A study by the US Geological Survey, the University of New Hampshire, and the Maine Department of Marine Resources showed that commercial mussel dragging poses a severe and long-lasting threat to eelgrass (Zostera marina). Dragging can damage large areas, with individual drag scars up to 79 acres in size found in Maine eelgrass beds. Dragging activity uproots eelgrass plants completely, removing leaves, rhizomes, and roots. Two independent methods were used to predict the rate of eelgrass recovery in heavily dragged areas. Under the best environmental conditions, complete revegetation of a dragged area would require an average of 11 years. Under conditions less favorable for eelgrass growth, such as reduced water quality, dragged areas could require more than 20 years to recover. Protection of eelgrass from commercial shellfish dragging will preserve important coastal habitat.</div></div>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20053054","usgsCitation":"Neckles, H.A., Short, F.T., Barker, S., and Kopp, B.S., 2005, Negative effects of commercial mussel dragging on eelgrass beds in Maine: U.S. Geological Survey Fact Sheet 2005-3054, 2 p., https://doi.org/10.3133/fs20053054.","productDescription":"2 p.","numberOfPages":"2","costCenters":[{"id":50464,"text":"Eastern Ecological Science Center","active":true,"usgs":true}],"links":[{"id":122441,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2005/3054/coverthb.jpg"},{"id":7148,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2005/3054/fs20053054.pdf","text":"Report","size":"8.46 MB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 2005-3054"}],"country":"United 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T.","contributorId":72078,"corporation":false,"usgs":true,"family":"Short","given":"Frederick","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":285333,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barker, Seth","contributorId":41536,"corporation":false,"usgs":true,"family":"Barker","given":"Seth","email":"","affiliations":[],"preferred":false,"id":285332,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kopp, Blaine S.","contributorId":99648,"corporation":false,"usgs":true,"family":"Kopp","given":"Blaine","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":285334,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":71014,"text":"sir20055164 - 2005 - Seepage study of McLeod Creek and East Canyon Creek near Park City, Summit County, Utah, 2004","interactions":[],"lastModifiedDate":"2019-12-30T13:55:59","indexId":"sir20055164","displayToPublicDate":"2005-08-13T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5164","title":"Seepage study of McLeod Creek and East Canyon Creek near Park City, Summit County, Utah, 2004","docAbstract":"Seepage investigations on McLeod Creek downstream of U.S. Geological Survey streamflow-gaging station McLeod Creek near Park City, Utah, and its confluence with Kimball Creek during the summer of 2004 indicate that this section of the creek is a gaining reach. The total seepage gains ranged from 1.8 to 2.7 cubic feet per second, or a 32 to 55 percent gain. The apparent average total seepage gain was 2.2 cubic feet per second, or an average 42 percent gain. Seepage investigations from the U.S. Geological Survey streamflow-gaging station at East Canyon Creek below I-80 Rest Stop near Park City, Utah, to the station at East Canyon Creek near Jeremy Ranch, Utah, indicate that this section of East Canyon Creek is a slightly losing reach. The total seepage losses ranged from -1.2 to -2.0 cubic feet per second. This is a loss of between -18 and -27 percent from discharge measured at the upstream gaging station. The apparent average total seepage loss for the reach was -1.0 cubic feet per second, or -18 percent. Seepage information also was obtained along East Canyon Creek by using water-temperature data recorded in three shallow streambed piezometers. Surface-water temperature also was recorded at these locations. These water-temperature profiles indicate a seepage loss at all three locations along East Canyon Creek. This seepage loss appears to decrease in September and October.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055164","collaboration":"Prepared in cooperation with the Snyderville Basin Water Reclamation District","usgsCitation":"Wilkowske, C., 2005, Seepage study of McLeod Creek and East Canyon Creek near Park City, Summit County, Utah, 2004: U.S. Geological Survey Scientific Investigations Report 2005-5164, iv, 26 p., https://doi.org/10.3133/sir20055164.","productDescription":"iv, 26 p.","numberOfPages":"33","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":192619,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6673,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5164/","linkFileType":{"id":5,"text":"html"}},{"id":334240,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5164/PDF/SIR2005_5164.pdf"}],"country":"United States","state":"Utah","county":"Summit County","city":"Park City","otherGeospatial":"East Canyon Creek, McLeod 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C.D.","contributorId":63050,"corporation":false,"usgs":true,"family":"Wilkowske","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":283490,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70980,"text":"ds117 - 2005 - Occurrence of selected pharmaceutical and non-pharmaceutical compounds, and stable hydrogen and oxygen isotope ratios, in a riverbank filtration study, Platte River, Nebraska, 2001 to 2003, Volume 1","interactions":[],"lastModifiedDate":"2022-09-30T19:39:57.783349","indexId":"ds117","displayToPublicDate":"2005-08-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"117","title":"Occurrence of selected pharmaceutical and non-pharmaceutical compounds, and stable hydrogen and oxygen isotope ratios, in a riverbank filtration study, Platte River, Nebraska, 2001 to 2003, Volume 1","docAbstract":"<p class=\"body\">Although studied extensively in recent years in Europe, the occurrence of endocrine disrupters and other organic wastewater compounds in the environment in the United States is not well documented. To better understand the efficiency of riverbank filtration with respect to endocrine disrupting compounds and to evaluate the use of riverbank filtration as an effective means of drinking-water treatment, a study was conducted during 2001-2003 by the U.S. Geological Survey, in cooperation with the U.S. Environmental Protection Agency and the City of Lincoln, at an established riverbank-filtration well field with horizontal collector wells and vertical wells. This study provides information that will be useful for (1)&nbsp;increased understanding of the processes and factors important in controlling the transport of endocrine disrupters, such as pesticides and pharmaceuticals during riverbank filtration, (2)&nbsp;better understanding of the physical and chemical processes that affect riverbank-filtration efficiency, and (3)&nbsp;managing the water resources of the eastern Platte River Basin. This report presents analytical methods and data collected during the study. Data are presented as generalized statistics and in figures showing temporal variations.</p><p class=\"body\">Sites from which water-quality samples were collected for this study included wastewater sites (a cattle feedlot lagoon, a hog confinement lagoon, and wastewater-treatment plant effluent), surface-water sites (Platte River, Salt Creek, and Loup Power Canal), ground-water sites (one collector well and three vertical wells), and drinking-water sites (raw and finished). Field water-quality properties were measured in samples from these sites.</p><p class=\"body\">Pharmaceutical compounds were detected often in the wastewater-treatment plant effluent. Surface and ground water showed low-level concentrations of pharmaceuticals. Finished drinking-water samples did not contain detectable concentrations of pharmaceuticals except for low levels of cotinine and caffeine. Antibiotics were found in some of the wastewater samples and twice in Salt Creek. Antibiotics were not detected in any samples from the Platte River or the well field.</p><p class=\"body\">Surface-water samples were analyzed for total organic carbon and ground-water samples were analyzed for dissolved organic carbon. Samples from all sites were analyzed for major ions. Herbicides commonly detected in surface, ground, and drinking water included acetachlor, alachlor, atrazine, and metolachlor as well as degradates of these compounds. Most of the samples from wastewater sites were found to contain predominantly acetamide degradates. High concentrations of several organic wastewater indicator compounds were detected at the wastewater sites and in Salt Creek. Several organic wastewater indicator compounds were detected multiple times in samples from the Platte River. Bromoform, a by-product of disinfection in the treatment plant, was found in samples from the finished drinking water.</p><p class=\"body\">Stable hydrogen isotope ratios show a range in seasonal variation of -73.6 per mill to -38.1 per mill relative to Vienna Standard Mean Ocean Water (VSMOW) reference water and -69.2 per mill to -46.5 per mill for surface water and ground water, respectively. Oxygen isotope ratios for surface-water samples varied between -9.86 per mill and -5.05 per mill. Stable oxygen isotope ratios of ground waters varied between -9.62 per mill and -5.81 per mill.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ds117","usgsCitation":"Vogel, J.R., Verstraeten, I., Coplen, T., Furlong, E., Meyer, M.T., and Barber, L.B., 2005, Occurrence of selected pharmaceutical and non-pharmaceutical compounds, and stable hydrogen and oxygen isotope ratios, in a riverbank filtration study, Platte River, Nebraska, 2001 to 2003, Volume 1: U.S. Geological Survey Data Series 117, v, 64 p., https://doi.org/10.3133/ds117.","productDescription":"v, 64 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":186639,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6637,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/2005/117/","linkFileType":{"id":5,"text":"html"}},{"id":407735,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73947.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Nebraska","otherGeospatial":"Platte River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.39198303222656,\n              40.9855999586963\n            ],\n            [\n              -96.25808715820312,\n              40.9855999586963\n            ],\n            [\n              -96.25808715820312,\n              41.10263873253247\n            ],\n            [\n              -96.39198303222656,\n              41.10263873253247\n            ],\n            [\n              -96.39198303222656,\n              40.9855999586963\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f29ff","contributors":{"authors":[{"text":"Vogel, J. R.","contributorId":21639,"corporation":false,"usgs":true,"family":"Vogel","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":283417,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Verstraeten, Ingrid M.","contributorId":61033,"corporation":false,"usgs":true,"family":"Verstraeten","given":"Ingrid M.","affiliations":[],"preferred":false,"id":283419,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coplen, T.B.","contributorId":34147,"corporation":false,"usgs":true,"family":"Coplen","given":"T.B.","affiliations":[],"preferred":false,"id":283418,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Furlong, E. T. 0000-0002-7305-4603","orcid":"https://orcid.org/0000-0002-7305-4603","contributorId":98346,"corporation":false,"usgs":true,"family":"Furlong","given":"E. T.","affiliations":[],"preferred":false,"id":283422,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Meyer, M. T.","contributorId":92279,"corporation":false,"usgs":true,"family":"Meyer","given":"M.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":283421,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Barber, L. B.","contributorId":64602,"corporation":false,"usgs":true,"family":"Barber","given":"L.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":283420,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70955,"text":"sir20055034 - 2005 - Mercury in the Grand Calumet River/Indiana Harbor Canal and Lake Michigan, Lake County, Indiana, August 2001 and May 2002","interactions":[],"lastModifiedDate":"2016-06-22T10:55:00","indexId":"sir20055034","displayToPublicDate":"2005-07-31T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5034","title":"Mercury in the Grand Calumet River/Indiana Harbor Canal and Lake Michigan, Lake County, Indiana, August 2001 and May 2002","docAbstract":"<p>Water samples from the Grand Calumet River/Indiana Harbor Canal and Lake Michigan in Lake County, Indiana, were collected and analyzed for mercury. Sampling was done with ultra-clean protocols, and mercury was analyzed by low-level methods during seasons of contrasting weather and streamflow conditions in August 2001 and May 2002.</p>\n<p>Total mercury concentrations in all the Grand Calumet River/Indiana Harbor Canal samples exceeded the 1.3 nanogram per liter Indiana water-quality standard for waters within the Great Lakes system. Total mercury concentrations in the Lake Michigan samples did not exceed the Indiana water-quality standard. Total mercury and methylmercury concentrations were larger in more samples collected during the wet-weather streamflow conditions in May 2002 than in samples collected during the dry-weather streamflow conditions in August 2001. The largest total mercury concentrations were in samples collected from the West Branch Grand Calumet River near wetlands and municipal-effluent outfalls (17.2 nanograms per liter) and in samples collected from the Indiana Harbor Canal near the confluence of the East Branch and West Branch Grand Calumet River (16.0 nanograms per liter).</p>\n<p>Particulate total mercury was the predominant form of total mercury detected in samples from the Grand Calumet River/Indiana Harbor Canal. Methylmercury concentrations were no more than 1.5 percent of the total mercury concentrations in August 2001 and no more than 6.2 percent in May 2002. Nearly all methylmercury was particulate and was correlated to concentrations of dissolved solids, total organic carbon, and sulfate. The estimated composition of most of the suspended solids in the water samples from the Grand Calumet River/ Indiana Harbor Canal was sediment larger than medium clay containing minimal organic carbon and plant matter. Total mercury loads in the Indiana Harbor Canal during the time of water sampling were as large as 703 milligrams per hour in August 2001 and 542 milligrams per hour in May 2002. As much as 21 percent of the instantaneous mercury load in some stream reaches could have come from ground-water discharge.</p>\n<p>Data from this study have implications for a Total Maximum Daily Load (TMDL) for mercury in the Grand Calumet River/Indiana Harbor Canal. Comparisons of data from this study with historical data do not show substantial changes in the distribution of mercury in the study area from 1994 through 2002. Treated municipal effluent had larger mercury concentrations than industrial effluent and presents a potential for larger mercury loads that could be controlled to achieve a TMDL, based on concentration. Mercury in ground-water discharge may be difficult to control to achieve a TMDL because of its diffuse and widespread distribution.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055034","collaboration":"Prepared in cooperation with the Indiana Department of Environmental Management","usgsCitation":"Risch, M.R., 2005, Mercury in the Grand Calumet River/Indiana Harbor Canal and Lake Michigan, Lake County, Indiana, August 2001 and May 2002: U.S. Geological Survey Scientific Investigations Report 2005-5034, 46 p., https://doi.org/10.3133/sir20055034.","productDescription":"46 p.","startPage":"1","endPage":"46","numberOfPages":"55","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":186191,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6610,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5034/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Indiana","county":"Lake County","otherGeospatial":"Grand Calumet River, Indiana Harbor Canal, Lake Michigan","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.54112243652342,\n              41.57641597789266\n            ],\n            [\n              -87.54112243652342,\n              41.71034202043942\n            ],\n            [\n              -87.21668243408203,\n              41.71034202043942\n            ],\n            [\n              -87.21668243408203,\n              41.57641597789266\n            ],\n            [\n              -87.54112243652342,\n              41.57641597789266\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624c8e","contributors":{"authors":[{"text":"Risch, Martin R. 0000-0002-7908-7887 mrrisch@usgs.gov","orcid":"https://orcid.org/0000-0002-7908-7887","contributorId":2118,"corporation":false,"usgs":true,"family":"Risch","given":"Martin","email":"mrrisch@usgs.gov","middleInitial":"R.","affiliations":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":27231,"text":"Indiana-Kentucky Water Science Center","active":true,"usgs":true},{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":283368,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70926,"text":"ofr20051192 - 2005 - Digital-elevation and surface-classification maps of the Fish Creek area, Harrison Bay quadrangle, northern Alaska","interactions":[],"lastModifiedDate":"2023-03-22T20:17:59.173378","indexId":"ofr20051192","displayToPublicDate":"2005-07-22T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1192","title":"Digital-elevation and surface-classification maps of the Fish Creek area, Harrison Bay quadrangle, northern Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051192","usgsCitation":"Mars, J.L., Garrity, C.P., Houseknecht, D.W., Amoroso, L., and Meares, D.C., 2005, Digital-elevation and surface-classification maps of the Fish Creek area, Harrison Bay quadrangle, northern Alaska: U.S. Geological Survey Open-File Report 2005-1192, Report: 10 p.; 3 Plates: 63 x 36 inches, https://doi.org/10.3133/ofr20051192.","productDescription":"Report: 10 p.; 3 Plates: 63 x 36 inches","onlineOnly":"Y","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":193335,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6586,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1192/","linkFileType":{"id":5,"text":"html"}},{"id":110570,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_72128.htm","linkFileType":{"id":5,"text":"html"},"description":"72128"}],"country":"United States","state":"Alaska","otherGeospatial":"Fish Creek area, Harrison Bay quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -153.4,\n              70.5\n            ],\n            [\n              -153.4,\n              70\n            ],\n            [\n              -150.9083,\n              70\n            ],\n            [\n              -150.9083,\n              70.5\n            ],\n            [\n              -153.4,\n              70.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64adee","contributors":{"authors":[{"text":"Mars, John L. jmars@usgs.gov","contributorId":3428,"corporation":false,"usgs":true,"family":"Mars","given":"John","email":"jmars@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":false,"id":283331,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garrity, Christopher P. 0000-0002-5565-1818 cgarrity@usgs.gov","orcid":"https://orcid.org/0000-0002-5565-1818","contributorId":644,"corporation":false,"usgs":true,"family":"Garrity","given":"Christopher","email":"cgarrity@usgs.gov","middleInitial":"P.","affiliations":[{"id":5061,"text":"National Cooperative Geologic Mapping and Landslide Hazards","active":true,"usgs":true},{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":283328,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Houseknecht, David W. 0000-0002-9633-6910 dhouse@usgs.gov","orcid":"https://orcid.org/0000-0002-9633-6910","contributorId":645,"corporation":false,"usgs":true,"family":"Houseknecht","given":"David","email":"dhouse@usgs.gov","middleInitial":"W.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":283329,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Amoroso, Lee lamoroso@usgs.gov","contributorId":3069,"corporation":false,"usgs":true,"family":"Amoroso","given":"Lee","email":"lamoroso@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":283330,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Meares, Donald C.","contributorId":94753,"corporation":false,"usgs":true,"family":"Meares","given":"Donald","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":283332,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70895,"text":"fs20053067 - 2005 - Using radar to understand migratory birds and their habitats: Critical needs for the Gulf of Mexico","interactions":[],"lastModifiedDate":"2016-09-15T11:00:07","indexId":"fs20053067","displayToPublicDate":"2005-07-18T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-3067","title":"Using radar to understand migratory birds and their habitats: Critical needs for the Gulf of Mexico","docAbstract":"<p>Nearly all Neotropical migratory landbird species of the eastern United States as well as many western species use Louisiana and the northern Gulf of Mexico coast during their transcontinental migrations each spring and fall. Radar has determined that hundreds of millions of birds make the nocturnal crossing of the Gulf of Mexico resulting in daily flights of as many as 2.5 million individuals stopping in Louisiana to feed and rest. These migration landings are so spectacular that the term “fallout” has been coined to describe the concentrations of birds arriving on the coast. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20053067","usgsCitation":"Smith, G.J., and Barrow, W., 2005, Using radar to understand migratory birds and their habitats: Critical needs for the Gulf of Mexico: U.S. Geological Survey Fact Sheet 2005-3067, 2 p., https://doi.org/10.3133/fs20053067.","productDescription":"2 p.","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":122400,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3067.jpg"},{"id":6546,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://archive.usgs.gov/archive/sites/www.nwrc.usgs.gov/factshts/2005-3067.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":10925,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://archive.usgs.gov/archive/sites/www.nwrc.usgs.gov/factshts/2005-3067/2005-3067.htm","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a16e4b07f02db603ca2","contributors":{"authors":[{"text":"Smith, Gregory J. gsmith@usgs.gov","contributorId":3436,"corporation":false,"usgs":true,"family":"Smith","given":"Gregory","email":"gsmith@usgs.gov","middleInitial":"J.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":283237,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barrow, Wylie 0000-0003-4671-2823","orcid":"https://orcid.org/0000-0003-4671-2823","contributorId":90684,"corporation":false,"usgs":true,"family":"Barrow","given":"Wylie","affiliations":[],"preferred":false,"id":283238,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70894,"text":"fs20053069 - 2005 - Migratory bird pathways and the Gulf of Mexico: Importance of Louisiana's coast","interactions":[],"lastModifiedDate":"2016-09-15T11:02:22","indexId":"fs20053069","displayToPublicDate":"2005-07-18T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-3069","title":"Migratory bird pathways and the Gulf of Mexico: Importance of Louisiana's coast","docAbstract":"<p>Because of its geographic position, Louisiana plays an important role in the hemispheric-scale phenomenon known as the Nearctic-Neotropical bird migration system. Each year millions of landbirds migrate across or near to the coast of the Gulf of Mexico. Birds migrate in large, broad fronts that sometimes exceed 2 million individuals, and there is an advantage for them to take a direct north-south route (the shortest distance).</p><ul><li>During migration seasons, nearly all of the migratory landbird species of the eastern United States, as well as many western species, use the coastal plains of the western gulf.</li><li>Spring migrants arrive with depleted energy reserves and depend on Louisiana's coastal habitats to provide food and cover after long gulf crossings.</li><li>Fall migrants depend on Louisiana’s coastal habitats for food to store fat reserves just prior to gulf crossings in autumn.</li><li>Mortality during the migratory period can be high. Recent research on the black-throated blue warbler (<i>Dendroica caerulescens</i>) indicates that more than 85% of the annual mortality for the species occurs during migration.<br></li></ul><p>Migrants en route tend to concentrate in habitats adjacent to ecological barriers; DOI land managers need to identify key coastal landscape features that are important to these birds.</p><p>Because of the vastness of the North American continent, it is nearly impossible to delineate movement patterns and migration pathways by using traditional ground-based surveys.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20053069","usgsCitation":"Smith, G.J., and Barrow, W., 2005, Migratory bird pathways and the Gulf of Mexico: Importance of Louisiana's coast: U.S. Geological Survey Fact Sheet 2005-3069, 1 p., https://doi.org/10.3133/fs20053069.","productDescription":"1 p.","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":126880,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3069.jpg"},{"id":6545,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://archive.usgs.gov/archive/sites/www.nwrc.usgs.gov/factshts/2005-3069.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":10926,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://archive.usgs.gov/archive/sites/www.nwrc.usgs.gov/factshts/2005-3069/2005-3069.htm","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635592","contributors":{"authors":[{"text":"Smith, Gregory J. gsmith@usgs.gov","contributorId":3436,"corporation":false,"usgs":true,"family":"Smith","given":"Gregory","email":"gsmith@usgs.gov","middleInitial":"J.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":283235,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barrow, Wylie 0000-0003-4671-2823","orcid":"https://orcid.org/0000-0003-4671-2823","contributorId":90684,"corporation":false,"usgs":true,"family":"Barrow","given":"Wylie","affiliations":[],"preferred":false,"id":283236,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70904,"text":"ofr20041455 - 2005 - Preliminary geologic map of the Hemet 7.5' quadrangle, Riverside County, California","interactions":[],"lastModifiedDate":"2022-04-14T18:48:36.445141","indexId":"ofr20041455","displayToPublicDate":"2005-07-18T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1455","title":"Preliminary geologic map of the Hemet 7.5' quadrangle, Riverside County, California","docAbstract":"<p>The Hemet 7.5' quadrangle is located near the eastern edge of the Perris block of the Peninsular Ranges batholith. The northeastern corner of the quadrangle extends across the San Jacinto Fault Zone onto the edge of the San Jacinto Mountains block. The Perris block is a relatively stable area located between the Elsinore Fault Zone on the west and the San Jacinto Fault Zone on the east. Both of the fault zones are active; the San Jacinto being the seismically most active in southern California. The fault zone is obscured by very young alluvial deposits. The concealed location of the San Jacinto Fault Zone shown on this quadrangle is after Sharp, 1967. The geology of the quadrangle is dominated by Cretaceous tonalite formerly included in the Coahuila Valley pluton of Sharp (1967). The northern part of Sharp's Coahuila Valley pluton is separated out as the Hemet pluton. Tonalite of the Hemet pluton is more heterogeneous than the tonalite of the Coahuila Valley pluton and has a different sturctural pattern. The Coahuila Valley pluton consists of relatively homogeneous hornblende-biotite tonalite, commonly with readily visible large euhedral honey-colored sphene crystals. Only the tip of the adjacent Tucalota Valley pluton, another large tonalite pluton, extends into the quadrangle. Tonalite of the Tucalota Valley pluton is very similar to the tonalite of the Coahuila Valley pluton except it generally lacks readily visible sphene. In the western part of the quadrangle a variety of amphibolite grade metasedimentary rocks are informally referred to as the rocks of Menifee Valley; named for exposures around Menifee Valley west of the Hemet quadrangle. In the southwestern corner of the quadrangle a mixture of schist and gneiss marks a suture that separated low metamorphic grade metasedimentary rocks to the west from high metamorphic grade rocks to the east. The age of these rocks is interpreted to be Triassic and the age of the suturing is about 100 Ma, essentially the same age as the adjacent Coahuila Valley pluton. Rocks within the suture zone consist of a mixture of lithologies from both sides of the suture. Gneiss, schist, and anatectic gneiss are the predominate lithologies within the rocks on the east side of the suture. Lesser amounts of metalithic greywacke and lenticular masses of black amphibolite are subordinate rock types. Biotite, biotite-sillimanite and lesser amounts of garnet-biotite-sillimanite schist and metaquartzite-metalithic greywacke lithologies occur west of the suture. Pleistocene continental beds, termed the Bautista beds occur east of the San Jacinto Fault Zone in the northeast corner of the quadrangle. Most of the Bautista beds were derived from the San Jacinto pluton that is located just to the east of the sedimentary rocks. Along the northern part of the quadrangle is the southern part of a large Holocene-late Pleistocene fan emanating from Baustista Canyon. Sediments in the Bautista fan are characterized by their content of detritus derived from amphibolite grade metasedimentary rocks located in the Bautista Canyon drainage. Between the Holocene-late Pleistocene Bautista fan and the Santa Rosa Hills is the remnant of a much older Bautista Canyon alluvial fan. A pronounced Holocene-late Pleistocene channel was developed along the south fringe of the very old alluvial fan and the Santa Rosa Hill. A now dissected late to middle Pleistocene alluvial complex was produced by the coalesced fans of Goodhart, St. Johns, and Avery canyons, and Cactus Valley. Pleistocene continental beds, termed the Bautista beds occur east of the San Jacinto Fault Zone in the northeast corner of the quadrangle. Most of the Bautista beds were derived from the San Jacinto pluton that is located just to the east of the sedimentary rocks. Along the northern part of the quadrangle is the southern part of a large Holocene-late Pleistocene fan emanating from Baustista Canyon.&nbsp;</p>","language":"English","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr20041455","usgsCitation":"Morton, D.M., and Matti, J.C., 2005, Preliminary geologic map of the Hemet 7.5' quadrangle, Riverside County, California (Version 1.1, Revised Mar 2008): U.S. Geological Survey Open-File Report 2004-1455, 1 Plate: 44 x 36 inches; ReadMe; Metadata; Data Files, https://doi.org/10.3133/ofr20041455.","productDescription":"1 Plate: 44 x 36 inches; ReadMe; Metadata; Data Files","additionalOnlineFiles":"Y","costCenters":[{"id":647,"text":"Western Earth Surface Processes","active":false,"usgs":true}],"links":[{"id":186419,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":398743,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_72184.htm"},{"id":6554,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1455/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","projection":"Polyconic","country":"United States","state":"California","county":"Riverside County","otherGeospatial":"Hemet 7.5' quadrangle,","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117,\n              33.625\n            ],\n            [\n              -116.875,\n              33.625\n            ],\n            [\n              -116.875,\n              33.75\n            ],\n            [\n              -117,\n              33.75\n            ],\n            [\n              -117,\n              33.625\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.1, Revised Mar 2008","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbf4b","contributors":{"authors":[{"text":"Morton, Douglas M. scamp@usgs.gov","contributorId":4102,"corporation":false,"usgs":true,"family":"Morton","given":"Douglas","email":"scamp@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":283262,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Matti, Jon C.","contributorId":24444,"corporation":false,"usgs":true,"family":"Matti","given":"Jon","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":283263,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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